Editing Baltic Sea

{{short description|Sea in northern Europe}}
{{Use dmy dates|date=February 2025}}
{{Use British English|date=January 2025}}
{{Infobox body of water
| name               = Baltic Sea region
| image              = The Baltic Sea.png
| image_size         = 287px
| caption            = Map of the Baltic Sea region
| alt                = Map
| image_bathymetry   = 
| caption_bathymetry = 50
| location           = [[Europe]]
| coords             = {{Coord|58|N|20|E|type:waterbody_region:XZ_scale:5000000|display=inline,title}} (slightly east of the north tip of Gotland Island)
| type               = [[Sea]]
| inflow             = [[Daugava River|Daugava]], [[Kemijoki]], [[Neman River|Neman]] (Nemunas), [[Neva]], [[Oder]], [[Vistula]], [[Lule River|Lule]], [[Narva River|Narva]], [[Torne älv|Torne]]
| outflow            = [[Danish straits]]
| catchment          = {{convert|1641650|km2|abbr=on}}
| basin_countries    = ''Coastal'': [[Denmark]], [[Estonia]], [[Finland]], [[Germany]], [[Latvia]], [[Lithuania]], [[Poland]], [[Russia]], [[Sweden]]<br/>''Non-coastal'': [[Belarus]], [[Czech Republic]], [[Norway]], [[Slovakia]], [[Ukraine]]<ref>{{cite web|title=Coalition Clean Baltic |url=http://www.ccb.se/newsletters/2005/07/map_final.jpg |access-date=5 July 2013 |url-status=dead |archive-url=https://web.archive.org/web/20130602044612/http://www.ccb.se/newsletters/2005/07/map_final.jpg |archive-date=2 June 2013}}</ref>
| length             = {{convert|1601|km|abbr=on}}
| width              = {{convert|193|km|abbr=on}}
| area               = {{convert|377000|km2|abbr=on}}
| depth              = {{convert|55|m|abbr=on}}
| max-depth          = {{convert|459|m|abbr=on}}
| volume             = {{convert|21700|km3|acre.ft|abbr=on}}
| residence_time     = 25 years
| salinity           = 
| shore              = {{convert|8000|km|abbr=on}}
| temperature_high   = 
| temperature_low    = 
| frozen             = 
| islands            = [[Abruka]], [[Aegna]], [[Archipelago Sea|Archipelago Sea Islands]] ([[Åland]]), [[Bornholm]], [[Dänholm]], [[Ertholmene]], [[Falster]], [[Fårö]], [[Fehmarn]], [[Gotland]], [[Hailuoto]], [[Hiddensee]], [[Hiiumaa]], [[Holmöarna]], [[Kassari]], [[Kesselaid]], [[Kihnu]], [[Kimitoön (island)|Kimitoön]], [[Kõinastu]], [[Kotlin Island|Kotlin]], [[Laajasalo]], [[Lauttasaari]], [[Lidingö]], [[Ljusterö]], [[Lolland]], [[Manilaid]], [[Mohni]], [[Møn]], [[Muhu]], [[Poel]], [[Prangli]], [[Osmussaar]], [[Öland]], [[Replot]], [[Ruhnu]], [[Rügen]], [[Saaremaa]], [[Stora Karlsö]], [[Suomenlinna]], [[Pakri Islands|Suur-Pakri and Väike-Pakri]], [[Ummanz]], [[Usedom|Usedom/Uznam]], [[Väddö]], [[Värmdö (island)|Värmdö]], [[Vilsandi]], [[Vormsi]], [[Wolin]]
| islands_category   = Baltic islands
| trenches           = 
| benches            = 
| cities             = [[Copenhagen]], [[Gdańsk]], [[Gdynia]], [[Greifswald]], [[Haapsalu]], [[Helsinki]], [[Jūrmala]], [[Kaliningrad]], [[Kiel]], [[Klaipėda]], [[Kołobrzeg]], [[Kuressaare]], [[Kärdla]], [[Lübeck]], [[Luleå]], [[Mariehamn]], [[Oulu]], [[Palanga]], [[Paldiski]], [[Pärnu]], [[Riga]], [[Rostock]], [[Saint Petersburg]], [[Liepāja]], [[Stockholm]], [[Tallinn]], [[Turku]], [[Ventspils]]
| reference          = <ref>{{cite book|url=https://books.google.com/books?id=r9CgJNV_6KAC&pg=PA75|title=Resilience and the Behavior of Large-Scale Systems|first1=Lance H.|last1=Gunderson|first2=Lowell|last2=Pritchard|date=1 October 2002|publisher=Island Press|via=Google Books|isbn=9781559639712}}</ref>
<!--
| map2 = File:Belte inter.png
| caption = Danish straits and southwestern Baltic Sea -->}}

The '''Baltic Sea''' is an arm of the [[Atlantic Ocean]] that is enclosed by the countries of [[Denmark]], [[Estonia]], [[Finland]], [[Germany]], [[Latvia]], [[Lithuania]], [[Poland]], [[Russia]], [[Sweden]], and the [[North European Plain|North]] and Central [[European Plain]] regions.<ref name=":3">{{Cite book |last=Niktalab |first=Poopak |author-link=Poopak NikTalab |title=Over the Alps: History of Children and Youth Literature in Europe |publisher=Faradid Publisher |year=2024 |isbn=9786225740457 |edition=1st |location=Tehran, Iran |pages=6 |language=fa}}</ref> It is the world's largest [[brackish water]] basin.

The sea stretches from 53°N to 66°N latitude and from 10°E to 30°E longitude. It is a [[Continental shelf#Shelf seas|shelf sea]] and [[marginal sea]] of the Atlantic with limited water exchange between the two, making it an [[inland sea]]. The Baltic Sea drains through the [[Danish straits]] into the [[Kattegat]] by way of the [[Øresund]], [[Great Belt]] and [[Little Belt]]. It includes the [[Gulf of Bothnia]] (divided into the [[Bothnian Bay]] and the [[Bothnian Sea]]), the [[Gulf of Finland]], the [[Gulf of Riga]] and the [[Bay of Gdańsk]].

The "[[Baltic Proper]]" is bordered on its northern edge, at latitude 60°N, by [[Åland]] and the Gulf of Bothnia, on its northeastern edge by the Gulf of Finland, on its eastern edge by the Gulf of Riga, and in the west by the Swedish part of the southern Scandinavian Peninsula.

The Baltic Sea is connected by [[Canal|artificial waterways]] to the [[White Sea]] via the [[White Sea–Baltic Canal]] and to the [[German Bight]] of the [[North Sea]] via the [[Kiel Canal]].

== Definitions ==
[[File:Hel in summer.jpg|thumb|[[Hel Peninsula]]]]
[[File:Belte inter.png|thumb|Danish straits and southwestern Baltic Sea]]
[[File:Karta öfver Åland.png|thumb|[[Åland]] between [[Baltic Proper]] and the [[Gulf of Bothnia]]]]

=== Administration ===
The [[Helsinki Convention on the Protection of the Marine Environment of the Baltic Sea Area]] includes the Baltic Sea and the [[Kattegat]], without calling Kattegat a part of the Baltic Sea, "For the purposes of this Convention the 'Baltic Sea Area' shall be the Baltic Sea and the Entrance to the Baltic Sea, bounded by the parallel of the Skaw in the Skagerrak at 57°44.43'N."<ref>{{cite web|url=http://www.helcom.fi/Documents/About%20us/Convention%20and%20commitments/Helsinki%20Convention/|title=Text of Helsinki Convention|access-date=26 April 2014|archive-url=https://archive.today/20140502201121/http://www.helcom.fi/Documents/About%20us/Convention%20and%20commitments/Helsinki%20Convention/|archive-date=2 May 2014|url-status=dead}}</ref>

===Traffic history===
Historically, the [[Kingdom of Denmark]] collected [[Sound Dues]] from ships at the border between the ocean and the land-locked Baltic Sea, in tandem: in the [[Øresund]] at [[Kronborg]] castle near [[Helsingør]]; in the [[Great Belt]] at [[Nyborg]]; and in the [[Little Belt]] at its narrowest part then [[Fredericia]], after that stronghold was built. The narrowest part of Little Belt is the "Middelfart Sund" near [[Middelfart]].<ref>{{Cite web|url=https://pierer.de-academic.com/66040/Sundzoll|title=Sundzoll|website=Academic dictionaries and encyclopedias|access-date=16 June 2022|archive-date=2 October 2022|archive-url=https://web.archive.org/web/20221002094240/https://pierer.de-academic.com/66040/Sundzoll|url-status=live}}</ref>

===Oceanography===
Geographers widely agree that the preferred physical border between the Baltic and North Seas is the Langelandsbælt (the southern part of the [[Great Belt]] strait near [[Langeland]]) and the [[Drogden]]-Sill strait.<ref>{{cite web|url=http://www.io-warnemuende.de/Antworten_Fragen_zum_Meer.html?frage=49|title=Fragen zum Meer (Antworten) – IOW|website=www.io-warnemuende.de|access-date=31 May 2023|archive-date=20 April 2014|archive-url=https://web.archive.org/web/20140420053829/http://www.io-warnemuende.de/Antworten_Fragen_zum_Meer.html?frage=49|url-status=live}}</ref> The Drogden Sill is situated north of [[Køge Bugt]] and connects [[Dragør]] in the south of [[Copenhagen]] to [[Malmö]]; it is used by the [[Øresund Bridge]], including the ''Drogden Tunnel''. By this definition, the [[Danish straits]] is part of the entrance, but the [[Bay of Mecklenburg]] and the [[Bay of Kiel]] are parts of the Baltic Sea.
Another usual border is the line between [[Falsterbo]], Sweden, and [[Stevns Klint]], Denmark, as this is the southern border of Øresund. It is also the border between the shallow southern Øresund (with a typical depth of 5–10 meters only) and notably deeper water.

===Hydrography and biology===
[[Drogden]] Sill (depth of {{convert|7|m|abbr=on}}) sets a limit to Øresund and [[Darss]] Sill (depth of {{convert|18|m|abbr=on}}), and a limit to the Belt Sea.<ref>{{Cite web |url=https://www.kemi.se/Documents/Publikationer/Trycksaker/PM/PM-9-12-BaltSens.pdf |title=Swedish Chemicals Agency (KEMI): The BaltSens Project – The sensitivity of the Baltic Sea ecosystems to hazardous compounds |access-date=26 April 2014 |archive-url=https://web.archive.org/web/20130530201134/http://kemi.se/Documents/Publikationer/Trycksaker/PM/PM-9-12-BaltSens.pdf |archive-date=30 May 2013 |url-status=dead }}</ref> The shallow [[Sill (geology)|sills]] are obstacles to the flow of heavy salt water from the Kattegat into the basins around [[Bornholm]] and [[Gotland]].

The Kattegat and the southwestern Baltic Sea are well oxygenated and have a rich biology. The remainder of the Sea is brackish, poor in oxygen, and in species. Thus, statistically, the more of the entrance that is included in its definition, the healthier the Baltic appears; conversely, the more narrowly it is defined, the more endangered its biology appears.

== Etymology and nomenclature ==
[[Tacitus]] called it the Suebic Sea, Latin: {{lang|la|Mare Suebicum}} after the [[Germanic people]] of the [[Suebi]],<ref>Tacitus, [[Germania (book)|''Germania'']]([http://www.thelatinlibrary.com/tacitus/tac.ger.shtml#45 online text] {{Webarchive|url=https://web.archive.org/web/20030418012844/http://www.thelatinlibrary.com/tacitus/tac.ger.shtml#45 |date=18 April 2003 }}): ''Ergo iam dextro Suebici maris litore Aestiorum gentes adluuntur, quibus ritus habitusque Sueborum, lingua Britannicae propior.''&nbsp;– "Upon the right of the Suevian Sea the Æstyan nations reside, who use the same customs and attire with the Suevians; their language more resembles that of Britain." ([http://www.gutenberg.org/files/2995/2995-h/2995-h.htm English text online] {{Webarchive|url=https://web.archive.org/web/20201201132636/http://www.gutenberg.org/files/2995/2995-h/2995-h.htm |date=1 December 2020 }})</ref><ref>{{Cite book |last=Benario |first=Herbert W. |url=https://books.google.com/books?id=ZHFvEAAAQBAJ&dq=Suebic+sea+baltic&pg=PA110 |title=Tacitus: Germania |date=1 July 1999 |publisher=Liverpool University Press |isbn=978-1-80034-609-3 |pages=110 |language=en |access-date=13 May 2023 |archive-date=13 May 2023 |archive-url=https://web.archive.org/web/20230513013524/https://books.google.com/books?id=ZHFvEAAAQBAJ&newbks=0&printsec=frontcover&pg=PA110&dq=Suebic+sea+baltic&hl=no |url-status=live }}</ref> and [[Ptolemy]] ''[[Sarmatians|Sarmatian]] Ocean'' after the [[Sarmatians]],<ref>Ptolemy, ''Geography'' III, chapter 5: "Sarmatia in Europe is bounded on the north by the Sarmatian ocean at the Venedic gulf" ([http://topostext.org/work.php?work_id=209 online text] {{Webarchive|url=https://web.archive.org/web/20170803094706/http://topostext.org/work.php?work_id=209 |date=3 August 2017 }}).</ref> but the first to name it the ''Baltic Sea'' ({{Langx|la-x-medieval|[[wikt:Mare Balticum|Mare Balticum]]}}) was the eleventh-century German chronicler [[Adam of Bremen]]. It might be connected to the Germanic word ''belt'', a name used for two of the Danish straits, [[the Belts]], while others claim it to be directly derived from the source of the Germanic word, [[Latin]] {{lang|la|balteus}} "belt".<ref name="Latin-etymology">{{in lang|sv}} [https://runeberg.org/nfbb/0435.html Balteus] {{Webarchive|url=https://web.archive.org/web/20210127092958/http://runeberg.org/nfbb/0435.html |date=27 January 2021 }} in ''[[Nordisk familjebok]]''.</ref> [[Adam of Bremen]] himself compared the sea with a belt, stating that it is so named because it stretches through the land as a belt (''Balticus, eo quod in modum baltei longo tractu per [[Scythians|Scithicas]] regiones tendatur usque in [[Ancient Greece|Greciam]]'').

He might also have been influenced by the name of a legendary island mentioned in the [[Natural History (Pliny)|''Natural History'']] of [[Pliny the Elder]]. Pliny mentions an island named ''[[Baltia]]'' (or ''Balcia'') with reference to accounts of [[Pytheas]] and [[Xenophon]]. It is possible that Pliny refers to an island named Basilia ("the royal") in ''On the Ocean'' by Pytheas. ''Baltia'' also might be derived from "belt", and therein mean "near belt of sea, strait".{{Citation needed|date=June 2024}}

Others have suggested that the name of the island originates from the [[Proto-Indo-European language|Proto-Indo-European]] root ''*bʰel'' meaning "white, fair",<ref>{{cite web|url=http://starling.rinet.ru/cgi-bin/response.cgi?single=1&basename=%2Fdata%2Fie%2Fpiet&text_number=+129&root=config|title=Indo-European etymology : Query result|date=25 February 2007|url-status=live |archive-url=https://web.archive.org/web/20070225150051/http://starling.rinet.ru/cgi-bin/response.cgi?single=1&basename=%2Fdata%2Fie%2Fpiet&text_number=+129&root=config|archive-date=25 February 2007}}</ref> which may echo the naming of seas after colours relating to the cardinal points (as per [[Black Sea]] and [[Red Sea]]).{{sfn|Schmitt|1989|pages=310–313}} This '*bʰel' root and basic meaning were retained in [[Lithuanian language|Lithuanian]] (as {{lang|lt|baltas}}), [[Latvian language|Latvian]] (as {{lang|lv|balts}}) and [[Slavic languages|Slavic]] (as {{lang|sla|bely}}). On this basis, a related hypothesis holds that the name originated from this Indo-European root via a [[Baltic language]] such as Lithuanian.<ref>{{cite book
| last = Forbes
| first = Nevill
| title = The Position of the Slavonic Languages at the present day
| publisher = [[Oxford University Press]]
| year = 1910
| page = 7
| url = https://archive.org/stream/positionslavoni00forbgoog#page/n9/mode/1up}}</ref> Another explanation is that, while derived from the aforementioned root, the name of the sea is related to names for various forms of water and related substances in several European languages, that might have been originally associated with colors found in swamps (compare Proto-Slavic ''[[wikt:Reconstruction:Proto-Slavic/bolto|*bolto]]'' "swamp"). Yet another explanation is that the name originally meant "enclosed sea, bay" as opposed to open sea.<ref name="baltu valodas">{{cite book |last=Dini |first=Pietro Umberto | title=Le lingue baltiche |year=1997 |publisher=La Nuova Italia |location=Florence |language=it |isbn=978-88-221-2803-4}}</ref>

In the [[Middle Ages]] the sea was known by a variety of names. The name Baltic Sea became dominant after 1600. Usage of ''Baltic'' and similar terms to denote the region east of the sea started only in the 19th century.{{Citation needed|date=June 2024}}

===Name in other languages===
The Baltic Sea was known in ancient Latin language sources as {{lang|la|Mare Suebicum}} or even {{lang|la|Mare Germanicum}}.<ref>Cfr. [[Hartmann Schedel]]'s 1493 ([[:File:Schedelsche Weltchronik d 287.jpg|map]]), where the Baltic Sea is called ''Mare Germanicum'', whereas the Northern Sea is called ''Oceanus Germanicus''.</ref> Older native names in languages that used to be spoken on the shores of the sea or near it usually indicate the geographical location of the sea (in Germanic languages), or its size in relation to smaller gulfs (in Old Latvian), or tribes associated with it (in Old Russian the sea was known as the Varanghian Sea). In modern languages, it is known by the equivalents of "East Sea", "West Sea", or "Baltic Sea" in different languages:
* "Baltic Sea" is used in Modern English; in the [[Baltic languages]] [[Latvian language|Latvian]] ({{lang|lv|Baltijas jūra}}; in Old Latvian it was referred to as "the Big Sea", while the present day Gulf of Riga was referred to as "the Little Sea") and [[Lithuanian language|Lithuanian]] ({{lang|lt|Baltijos jūra}}); in [[Latin]] ({{lang|la|Mare Balticum}}) and the [[Romance languages]] [[French language|French]] ({{lang|fr|Mer Baltique}}), [[Italian language|Italian]] ({{lang|it|Mar Baltico}}), [[Portuguese language|Portuguese]] ({{lang|pt|Mar Báltico}}), [[Romanian language|Romanian]] ({{lang|ro|Marea Baltică}}) and [[Spanish language|Spanish]] ({{lang|es|Mar Báltico}}); in [[Greek language|Greek]] ({{lang|el|Βαλτική Θάλασσα}} {{lang|el-latn|Valtikí Thálassa}}); in [[Albanian language|Albanian]] ({{lang|sq|Deti Balltik}}); in [[Welsh language|Welsh]] ({{lang|cy|Môr Baltig}}); in the [[Slavic languages]] [[Polish language|Polish]] ({{lang|pl|Morze Bałtyckie}} or {{lang|pl|Bałtyk}}), [[Czech language|Czech]] ({{lang|cs|Baltské moře}} or {{lang|cs|Balt}}), [[Slovenian language|Slovenian]] ({{lang|sl|Baltsko morje}}), [[Bulgarian language|Bulgarian]] ({{lang|bg|Балтийско море}} {{lang|bg-latn|Baltijsko More}}), [[Kashubian language|Kashubian]] ({{lang|csb|Bôłt}}), [[Macedonian language|Macedonian]] ({{lang|mk|Балтичко Море|italic=no}} {{lang|mk-latn|Baltičko More}}), [[Ukrainian language|Ukrainian]] ({{lang|uk|Балтійське море}} {{lang|uk-latn|Baltijs′ke More}}), [[Belarusian language|Belarusian]] ({{lang|be|Балтыйскае мора|italic=no}} {{lang|be-latn|Baltyjskaje Mora}}), [[Russian (language)|Russian]] ({{lang|ru|Балтийское море}} {{lang|ru-latn|Baltiyskoye More}}) and [[Serbo-Croatian]] ({{lang|sh|Baltičko more}} / {{lang|sr-Cyrl|Балтичко море}}); in [[Hungarian language|Hungarian]] ({{lang|hu|Balti-tenger}}).
* In [[Germanic languages]], except English, "East Sea" is used, as in [[Afrikaans]] ({{lang|af|Oossee}}), [[Danish language|Danish]] ({{lang|da|Østersøen}} {{IPA|da|ˈøstɐˌsøˀn̩|}}), [[Dutch language|Dutch]] ({{lang|nl|Oostzee}}), [[German language|German]] ({{lang|de|Ostsee}}), [[Low German]] ({{lang|nds|Oostsee}}), [[Icelandic language|Icelandic]] and [[Faroese language|Faroese]] ({{lang|is|Eystrasalt}}), [[Norwegian language|Norwegian]] ([[Bokmål]]: {{lang|nb|Østersjøen}} {{IPA|no|ˈø̂stəˌʂøːn|}}; [[Nynorsk]]: {{lang|nn|Austersjøen}}), and [[Swedish language|Swedish]] ({{lang|sv|Östersjön}}). In [[Old English]] it was known as {{lang|ang|Ostsǣ}},<ref>The [[Old English Orosius]]</ref> which does not however mean 'east sea' and may be related to a people known in the same work as the ''Osti''.<ref>Portham, 1880, p61</ref> Also in [[Hungarian language|Hungarian]] the former name was {{lang|hu|Keleti-tenger}} ("East-sea", due to German influence). In addition, [[Finnish language|Finnish]], a [[Finnic languages|Finnic language]], uses the term {{lang|fi|Itämeri}} "East Sea", possibly a [[calque]] from a Germanic language. As the Baltic is not particularly eastward in relation to Finland, the use of this term may be a leftover from the period of Swedish rule.
* In another Finnic language, [[Estonian language|Estonian]], it is called the "West Sea" ({{lang|et|Läänemeri}}), with the correct geography (the sea is west of Estonia). In [[South Estonian]], it has the meaning of both "West Sea" and "Evening Sea" (''Õdagumeri''). In the endangered [[Livonian language]] of Latvia, the sea (and sometimes the [[Irbe Strait]] as well) is called the "Large Sea" ({{lang|liv|Sūŗ meŗ}} or {{lang|liv|Sūr meŗ}}).<ref>{{Cite web |title=Livones.net - Burājot lībiešu jūrā: debespušu nosaukumi lībiešu valodā |url=http://www.livones.net/lv/norises/2021/burajot-libiesu-jura-debespusu-nosaukumi-libiesu-valoda |access-date=20 July 2023 |website=www.livones.net |language=en |archive-date=20 July 2023 |archive-url=https://web.archive.org/web/20230720221923/http://www.livones.net/lv/norises/2021/burajot-libiesu-jura-debespusu-nosaukumi-libiesu-valoda |url-status=live }}</ref><ref>{{Cite web |url=https://www.visit.dundaga.lv/userfiles/files/546/Livoniancoast_En2020.pdf |title=A JOURNEY ALONG THE LIVONIAN COAST / REIZ PIDS LĪVÕD RANDÕ |access-date=20 July 2023 |archive-date=20 July 2023 |archive-url=https://web.archive.org/web/20230720223044/https://www.visit.dundaga.lv/userfiles/files/546/Livoniancoast_En2020.pdf |url-status=live }}</ref>

== History ==
===Classical world===
At the time of the [[Roman Empire]], the Baltic Sea was known as the {{lang|la|Mare Suebicum}} or ''Mare Sarmaticum''. [[Gaius Cornelius Tacitus|Tacitus]] in his AD&nbsp;98 ''Agricola'' and ''Germania'' described the Mare Suebicum, named for the [[Suebi]] tribe, during the spring months, as a [[brackish]] sea where the ice broke apart and chunks floated about. The Suebi eventually migrated southwest to temporarily reside in the Rhineland area of modern Germany, where their name survives in the historic region known as [[Swabia]]. [[Jordanes]] called it the ''Germanic Sea'' in his work, the ''[[Getica]]''.{{Citation needed|date=June 2024}}

===Middle Ages===
[[File:Putgarten, Kap Arkona (2011-05-21) 3.JPG|thumb|[[Cape Arkona]] on the island of [[Rügen]] in Germany, was a sacred site of the [[Rani (Slavic tribe)|Rani]] tribe before Christianization.]]
In the early [[Middle Ages]], Norse (Scandinavian) merchants built a trade empire all around the Baltic. Later, the Norse fought for control of the Baltic against [[Wends|Wendish tribes]] dwelling on the southern shore. The Norse also used the rivers of [[Russia]] for trade routes, finding their way eventually to the [[Black Sea]] and southern Russia. This Norse-dominated period is referred to as the [[Viking Age]].{{Citation needed|date=June 2024}}

Since the [[Viking Age]], the Scandinavians have referred to the Baltic Sea as ''Austmarr'' ("Eastern Sea"). "Eastern Sea", appears in the ''[[Heimskringla]]'' and ''Eystra salt'' appears in ''[[Sörla þáttr]]''. [[Saxo Grammaticus]] recorded in ''[[Gesta Danorum]]'' an older name, ''[[Gandvik]]'', ''-vik'' being [[Old Norse]] for "bay", which implies that the Vikings correctly regarded it as an inlet of the sea. Another form of the name, "Grandvik", attested in at least one English translation of ''Gesta Danorum'', is likely to be a misspelling.{{Citation needed|date=June 2024}}

In addition to fish the sea also provides [[amber]], especially from its southern shores within today's borders of [[Poland]], [[Russia]] and [[Lithuania]]. First mentions of amber deposits on the South Coast of the Baltic Sea date back to the 12th century.<ref>[https://leta.st/blog/2016/07/history-of-russian-amber-1/ "The History of Russian Amber, Part 1: The Beginning"] {{Webarchive|url=https://web.archive.org/web/20180315013751/https://leta.st/blog/2016/07/history-of-Russian-amber-1/ |date=15 March 2018 }}, Leta.st</ref> The bordering countries have also traditionally exported lumber, [[Pine tar|wood tar]], [[flax]], [[hemp]] and furs by ship across the Baltic. Sweden had from early medieval times exported [[iron]] and [[silver]] mined there, while Poland had and still has extensive [[salt]] mines. Thus, the Baltic Sea has long been crossed by much merchant shipping.{{Citation needed|date=June 2024}}

The lands on the Baltic's eastern shore were among the last in Europe to be converted to [[Christianity]]. This finally happened during the [[Northern Crusades]]: [[Finland]] in the twelfth century by Swedes, and what are now [[Estonia]] and [[Latvia]] in the early thirteenth century by Danes and Germans ([[Livonian Brothers of the Sword]]). The [[Teutonic Order]] gained control over parts of the southern and eastern shore of the Baltic Sea, where they set up [[Monastic state of the Teutonic Knights|their monastic state]]. [[Lithuania]] was [[Christianization of Lithuania|the last European state to convert to Christianity]].{{Citation needed|date=June 2024}}

===An arena of conflict===
[[File:Haupthandelsroute Hanse.png|thumb|Main trading routes of the [[Hanseatic League]] (''Hanse'').]]

In the period between the 8th and 14th centuries, there was much piracy in the Baltic from the coasts of [[Pomerania]] and [[Prussia]], and the [[Victual Brothers]] held [[Gotland]].{{Citation needed|date=June 2024}}

Starting in the 11th century, the southern and eastern shores of the Baltic were settled by migrants mainly from [[Germany]], a movement called the ''[[Ostsiedlung]]'' ("east settling"). Other settlers were from the [[Netherlands]], [[Denmark]], and [[Scotland]]. The [[Polabian Slavs]] were gradually assimilated by the Germans.<ref>[https://www.britannica.com/EBchecked/topic/639735/Wend Wend – West Wend] {{Webarchive|url=https://web.archive.org/web/20141022135757/http://www.britannica.com/EBchecked/topic/639735/Wend |date=22 October 2014 }}. Britannica. Retrieved on 23 June 2011.</ref> [[Denmark]] gradually gained control over most of the Baltic coast, until she lost much of her possessions after being defeated in the 1227 [[Battle of Bornhöved (1227)|Battle of Bornhöved]].{{Citation needed|date=June 2024}}
[[File:Eerste fase van de Zeeslag in de Sont - First phase of the Battle of the Sound - November 8 1658 (Jan Abrahamsz Beerstraten, 1660).jpg|thumb|The naval [[Battle of the Sound]] took place on 8 November 1658 during the [[Dano-Swedish War (1658–60)|Dano-Swedish War]].]]
[[File:Admiralty Chart No 259 Baltic Sea, Published 1919.jpg|thumb|Nautical chart of the Baltic Sea in 1919.]]
[[File:Cap Arcona burning.jpg|thumb|The burning ''[[Cap Arcona]]'' shortly after the attacks, 3 May 1945. Only 350 survived of the 4,500 prisoners who had been aboard]]

In the 13th to 16th centuries, the strongest economic force in Northern Europe was the [[Hanseatic League]], a federation of merchant cities around the Baltic Sea and the [[North Sea]]. In the sixteenth and early seventeenth centuries, [[Polish–Lithuanian Commonwealth|Poland]], [[Denmark]], and [[Sweden]] fought wars for ''[[Dominium maris baltici]]'' ("Lordship over the Baltic Sea"). Eventually, it was Sweden that [[Swedish Empire|virtually encompassed the Baltic Sea]]. In Sweden, the sea was then referred to as ''Mare Nostrum Balticum'' ("Our Baltic Sea"). The goal of Swedish warfare during the 17th century was to make the Baltic Sea an all-Swedish sea (''Ett Svenskt innanhav''), something that was accomplished except the part between Riga in Latvia and [[Szczecin|Stettin]] in Pomerania. However, the [[Dutch Republic|Dutch]] dominated the Baltic trade in the seventeenth century.{{Citation needed|date=June 2024}}

In the eighteenth century, [[Russian Empire|Russia]] and [[Prussia]] became the leading powers over the sea. Sweden's defeat in the [[Great Northern War]] brought Russia to the eastern coast. Russia became and remained a dominating power in the Baltic. Russia's [[Peter I of Russia|Peter the Great]] saw the strategic importance of the Baltic and decided to found his new capital, [[Saint Petersburg]], at the mouth of the [[Neva]] river at the east end of the [[Gulf of Finland]]. There was much trading not just within the Baltic region but also with the North Sea region, especially eastern [[England]] and the [[Netherlands]]: their fleets needed the Baltic timber, tar, flax, and hemp.{{Citation needed|date=June 2024}}

During the [[Crimean War]], a joint British and French fleet attacked the Russian fortresses in the Baltic; the case is also known as the [[Åland War]]. They bombarded [[Sveaborg]], which guards [[Helsinki]]; and [[Kronstadt, Russia|Kronstadt]], which guards Saint Petersburg; and they destroyed [[Bomarsund, Åland|Bomarsund]] in [[Åland]]. After the unification of [[Germany]] in 1871, the whole southern coast became German. [[World War I]] was partly fought in the Baltic Sea. After 1920 [[Poland]] was granted access to the Baltic Sea at the expense of Germany by the [[Polish Corridor]] and enlarged the port of [[Gdynia]] in rivalry with the port of the [[Free City of Danzig]].{{Citation needed|date=June 2024}}

After the Nazis' rise to power, Germany reclaimed the [[Memelland]] and after the outbreak of the [[Eastern Front (World War II)]] occupied the Baltic states. In 1945, the Baltic Sea became a mass grave for retreating soldiers and refugees on torpedoed [[Operation Hannibal|troop transports]]. The sinking of the ''[[Wilhelm Gustloff (ship)|Wilhelm Gustloff]]'' remains the worst maritime disaster in history, killing (very roughly) 9,000 people. In 2005, a Russian group of scientists found over five thousand airplane wrecks, sunken warships, and other material, mainly from World War II, on the bottom of the sea.{{Citation needed|date=June 2024}}

===Since World War II===
Since the end of [[World War II]], various nations, including the [[Soviet Union]], the United Kingdom and the United States have disposed of [[Chemical warfare|chemical weapons]] in the Baltic Sea, raising concerns of environmental contamination.<ref>[http://www.dw-world.de/dw/article/0,,3102728,00.html Chemical Weapon Time Bomb Ticks in the Baltic Sea] {{Webarchive|url=https://web.archive.org/web/20120124021629/http://www.dw-world.de/dw/article/0,,3102728,00.html |date=24 January 2012 }} ''Deutsche Welle'', 1 February 2008.</ref> Today, fishermen occasionally find some of these materials: the most recent available report from the Helsinki Commission notes that four small scale catches of chemical munitions representing approximately {{convert|105|kg|abbr=on}} of material were reported in 2005. This is a reduction from the 25 incidents representing {{convert|1110|kg|abbr=on}} of material in 2003.<ref>[http://www.helcom.fi/stc/files/Publications/Proceedings/bsep112.pdf Activities 2006: Overview] {{webarchive |url=https://web.archive.org/web/20090114011006/http://www.helcom.fi/stc/files/Publications/Proceedings/bsep112.pdf |date=14 January 2009 }} Baltic Sea Environment Proceedings No. 112. [[Baltic Marine Environment Protection Commission|Helsinki Commission]].</ref> Until now, the [[U.S. Government]] refuses to disclose the exact coordinates of the wreck sites. Deteriorating bottles leak [[mustard gas]] and other substances, thus slowly poisoning a substantial part of the Baltic Sea.{{Citation needed|date=June 2024}}

After 1945, the [[Flight and expulsion of Germans (1944–1950)|German population was expelled]] from all areas east of the [[Oder-Neisse line]], [[Ethnic cleansing|making room]] for new Polish and Russian settlement. Poland [[Former eastern territories of Germany|gained most of the southern shore]]. The Soviet Union gained another access to the Baltic with the [[Kaliningrad Oblast]], that had been part of German-settled [[East Prussia]]. The Baltic states on the eastern shore were annexed by the Soviet Union. The Baltic then separated opposing military blocs: [[NATO]] and the [[Warsaw Pact]]. Neutral Sweden developed [[incident weapon]]s to defend its [[territorial waters]] after the [[Swedish submarine incidents]].<ref>{{cite journal |last=Ellis |first=M.G.M.W. |year=1986 |title=Sweden's Ghosts? |journal=Proceedings |volume=112 |issue=3 |pages=95–101 |publisher=[[United States Naval Institute]] }}</ref> This border status restricted trade and travel. It ended only after the collapse of the [[Communist]] regimes in Central and Eastern Europe in the late 1980s.
[[File:MM10249.jpg|thumb|right|In 1981, the [[Soviet submarine S-363|Soviet submarine ''S-363'']] ran on ground deep inside Swedish territorial waters, an incident which illustrated the impact of the [[Cold War]] on the Baltic Sea.]] 
Finland and Sweden joined NATO in 2023 and 2024, respectively, making the Baltic Sea almost entirely surrounded by the alliance's members, leading some commentators to label the sea a "NATO lake".<ref name="Kirby 2023">{{cite web | last=Kirby | first=Paul | title=Nato's border with Russia doubles as Finland joins | website=BBC News | date=4 April 2023 | url=https://www.bbc.com/news/world-europe-65173043 | access-date=5 April 2023 | archive-date=4 April 2023 | archive-url=https://web.archive.org/web/20230404150315/https://www.bbc.com/news/world-europe-65173043 | url-status=live }}</ref><ref name="RFI 2024 i241">{{cite web | title=Does Sweden joining make the Baltic Sea a 'NATO lake'? | website=RFI | date=26 February 2024 | url=https://www.rfi.fr/en/international-news/20240226-does-sweden-joining-make-the-baltic-sea-a-nato-lake | access-date=29 April 2024}}</ref><ref name="France 24 2024 r479">{{cite web | title=No longer neutral waters: What Baltic Sea strategy for Sweden after NATO enlargement? | website=France 24 | date=28 March 2024 | url=https://www.france24.com/en/tv-shows/the-debate/20240328-no-longer-neutral-waters-what-baltic-sea-strategy-for-sweden-after-nato-enlargement | access-date=29 April 2024}}</ref><ref name="Financial Times n260">{{cite news|last1=Milne|first1=Richard|last2=Seddon|first2=Max|url=https://www.ft.com/content/c6375406-df00-4e1d-801f-9435b6a8d253|title=Sweden joins 'Nato lake' on Moscow's doorstep|newspaper=[[Financial Times]]|date=7 March 2024|access-date=7 March 2024}}</ref><ref name="Kayali 2023 y072">{{cite web | last=Kayali | first=Laura | title=Sorry Russia, the Baltic Sea is NATO's lake now | website=POLITICO | date=13 July 2023 | url=https://www.politico.eu/article/nato-lake-what-sweden-and-finland-will-change-in-the-baltics-russia-ukraine-war/ | access-date=29 April 2024}}</ref> However, the legal status of the sea has not changed and it is still open to all nations.<ref>{{Cite web |title=No, Don’t Call the Baltic a ‘NATO Lake’ |url=https://www.rusi.orghttps//www.rusi.org |access-date=2025-06-01 |website=www.rusi.orghttps |language=en}}</ref> Such an arrangement has also existed for the [[European Union]] (EU) since May 2004 following the accession of the Baltic states and Poland. The remaining non-NATO and non-EU shore areas are Russian: the Saint Petersburg area and the [[Kaliningrad Oblast]] [[exclave]].

The Baltic Sea today is of significant economic and security importance due to its dense network of [[submarine cable]]s, [[Submarine pipeline|energy pipelines]], ports and offshore energy platforms. In recent years, there have been a number of incidents of sabotage in the Baltic Sea, resulting in damage to [[critical infrastructure]]s.<ref>{{Cite journal |last1=Blokus-Roszkowska |first1=Agnieszka |last2=Bogalecka |first2=Magda |last3=Kołowrocki |first3=Krzysztof |date=2016 |title=Critical infrastructure networks at Baltic Sea and its seaside |url=https://yadda.icm.edu.pl/baztech/element/bwmeta1.element.baztech-9c0fd253-9dc4-4947-8003-604c6a9f80f5 |journal=Journal of Polish Safety and Reliability Association |volume=7 |issue=2 |pages=7–14}}</ref><ref>Storgard, J. et al. (2025) ''Scenarios for the development of maritime safety and security in the Baltic Sea region''. Turku: Centre for Maritime Studies, University of Turku. Available at: <nowiki>https://mc.nato.int/media-centre/news/2025/nato-baltic-sentry-steps-up-patrols-in-the-baltic-sea-to-safeguard-critical-undersea-infrastructure.aspx</nowiki>.</ref><ref>{{Cite journal |last1=Bueger |first1=Christian |last2=Liebetrau |first2=Tobias |date=2023 |title=Critical maritime infrastructure protection: What's the trouble? |url=https://linkinghub.elsevier.com/retrieve/pii/S0308597X23003056 |journal=Marine Policy |language=en |volume=155 |issue=105772 |pages= |doi=10.1016/j.marpol.2023.105772|bibcode=2023MarPo.15505772B }}</ref> The most notable incidents include the [[Nord Stream pipelines sabotage]] in 2022, where a series of underwater explosions destroyed both [[Nord Stream|Nord Stream 1 and 2]].<ref>{{Cite journal |last=de Jong |first=Moniek |date=2024 |title=Tracing the downfall of the Nord Stream 2 gas pipeline |url=https://wires.onlinelibrary.wiley.com/doi/10.1002/wene.502 |journal=WIREs Energy and Environment |language=en |volume=13 |issue=1 |pages=e502 |doi=10.1002/wene.502 |bibcode=2024WIREE..13E.502D |issn=2041-840X}}</ref> In 2023, there was another incident involving the [[Balticconnector]] gas pipeline and a nearby data cable, which were damaged by the [[Hong Kong]]-flagged container ship [[Newnew Polar Bear|NewNew Polar Bear]].<ref>{{Citation |last1=Ringbom |first1=Henrik |title=Sabotage of Critical Offshore Infrastructure: a Case Study of the Balticconnector Incident |date=2024-07-27 |work=Maritime Security Law in Hybrid Warfare |pages=155–194 |url=https://brill.com/edcollchap/book/9789004707993/BP000019.xml |access-date=2025-05-25 |publisher=Brill Nijhoff |language=en |isbn=978-90-04-70799-3 |last2=Lott |first2=Alexander}}</ref><ref>{{Cite web |date=2025-05-09 |title=China detains captain of ship connected to Balticconnector damage |url=https://yle.fi/a/74-20160915 |access-date=2025-05-25 |website=Yle |language=en}}</ref>

Other significant incidents include the recent damage to several [[Submarine communications cable|undersea communication cables]]. The most recent incident of relevance was the [[2024 Estlink 2 incident|rupture of the Estlink 2 cable]] in late 2024. It is suspected that the oil tanker [[Eagle S]], believed to be part of a [[Russian shadow fleet]], is responsible.<ref>{{Cite web |date=2024-12-26 |title=Estlink cable disruption: Finnish Border Guard detains tanker linked to Russia's 'dark fleet' |url=https://yle.fi/a/74-20133516 |access-date=2025-05-25 |website=Yle |language=en}}</ref>

These events followed a series of responses from both [[NATO]] and the [[European Union|EU]]. In response, NATO Baltic Sea states have increased their [[Navy|naval]] presence in the Baltic Sea, and the NATO operation [[:de:NATO-Operation Baltic Sentry|Baltic Sentry]] was established. Simultaneously, the EU has implemented a series of measures designed to enhance the protection of critical maritime infrastructure. The EU has also underscored the commitment to strengthening cooperation with NATO.<ref>{{Cite web |last=NDR |title=Wieder Sabotage in der Ostsee? Erneut Datenkabel zwischen Finnland und Deutschland beschädigt - Schweden ermittelt |url=https://www.ndr.de/nachrichten/mecklenburg-vorpommern/Datenkabel-in-der-Ostsee-Schweden-ermittelt-wegen-Sabotage,kabelsabotage106.html |access-date=2025-05-25 |website=www.ndr.de |language=de}}</ref>

===Storms and storm floods===

Winter storms begin arriving in the region during October. These have caused numerous [[shipwreck]]s, and contributed to the extreme difficulties of rescuing passengers of the ferry [[MS Estonia|MS ''Estonia'']] en route from [[Tallinn]], Estonia, to [[Stockholm]], Sweden, in September 1994, which claimed the lives of 852 people. Older, wood-based shipwrecks such as the ''[[Vasa (ship)|Vasa]]'' tend to remain well-preserved, as the Baltic's cold and brackish water does not suit the [[shipworm]].

[[Storm surge]] floods are generally taken to occur when the water level is more than one metre above normal. In Warnemünde about 110 floods occurred from 1950 to 2000, an average of just over two per year.<ref>{{cite journal |url=http://www.ikzm-d.de/infos/pdfs/129_Bericht_Sturmfluten.pdf |title=Sturmfluten in der südlichen Ostsee (Westlicher und mittlerer Teil) |trans-title=Storm floods in the Southern Baltic (western and central part) |language=de |year=2005 |issue=39 |journal=Berichte des Bundesamtes für Seeschifffahrt und Hydrographie |page=6 |first1=Marzenna |last1=Sztobryn |first2=Hans-Joachim |last2=Stigge |first3=Danuta |last3=Wielbińska |first4=Bärbel |last4=Weidig |first5=Ida |last5=Stanisławczyk |first6=Alicja |last6=Kańska |first7=Katarzyna |last7=Krzysztofik |first8=Beata |last8=Kowalska |first9=Beata |last9=Letkiewicz |first10=Monika |last10=Mykita |access-date=2 July 2012 |archive-url=https://web.archive.org/web/20121028010502/http://www.ikzm-d.de/infos/pdfs/129_Bericht_Sturmfluten.pdf |archive-date=28 October 2012 |url-status=dead }}</ref>

Historic flood events were the [[All Saints' Flood of 1304]] and other floods in the years 1320, 1449, 1625, 1694, 1784 and 1825. Little is known of their extent.<ref>{{cite web |url=http://www.ikzm-d.de/inhalt.php?page=129,2843 |title=Sturmfluten an der Ostseeküste – eine vergessene Gefahr? |trans-title=Storm floods along the Baltic Sea coastline – a forgotten threat? |work=Informations-, Lern-, und Lehrmodule zu den Themen Küste, Meer und Integriertes Küstenzonenmanagement |publisher=EUCC Die Küsten Union Deutschland e. V. |access-date=2 July 2012 |archive-url=https://web.archive.org/web/20140724062335/http://www.ikzm-d.de/inhalt.php?page=129,2843 |archive-date=24 July 2014 |url-status=dead }} Citing {{cite book|last=Weiss |first=D. |chapter=Schutz der Ostseeküste von Mecklenburg-Vorpommern |editor-last=Kramer |editor-first=J. |editor2-first=H. |editor2-last=Rohde |title=Historischer Küstenschutz: Deichbau, Inselschutz und Binnenentwässerung an Nord- und Ostsee |trans-title=Historical coastal protection: construction of dikes, insular protection and inland drainage at North Sea and Baltic Sea | pages= 536–567 |location=Stuttgart |publisher=Wittwer |language=de}}</ref> From 1872, there exist regular and reliable records of water levels in the Baltic Sea. The highest was the [[1872 Baltic Sea flood|flood of 1872]] when the water was an average of {{convert|2.43|m|abbr=on}} above sea level at Warnemünde and a maximum of {{convert|2.83|m|abbr=on}} above sea level in Warnemünde. In the last very heavy floods the average water levels reached {{convert|1.88|m|abbr=on}} above sea level in 1904, {{convert|1.89|m|abbr=on}} in 1913, {{convert|1.73|m|abbr=on}} in January 1954, {{convert|1.68|m|abbr=on}} on 2–4 November 1995 and {{convert|1.65|m|abbr=on}} on 21 February 2002.<ref>{{cite web |url=http://www.ikzm-d.de/showaddon.php?text=386 |title=Sturmfluten an der deutschen Ostseeküste |trans-title=Storm floods at the German Baltic Sea coasts |first=Reiner |last=Tiesel |date=October 2003 |language=de |work=Informations-, Lern-, und Lehrmodule zu den Themen Küste, Meer und Integriertes Küstenzonenmanagement |publisher=EUCC Die Küsten Union Deutschland e. V. |access-date=2 July 2012 |archive-url=https://web.archive.org/web/20121012062254/http://www.ikzm-d.de/showaddon.php?text=386 |archive-date=12 October 2012 |url-status=dead }}</ref>

== Geography ==
=== Geophysical data ===
[[File:Baltic drainage basins (catchment area).svg|thumb|Baltic drainage basins (catchment area), with depth, elevation, major rivers and lakes]]
[[File:Curonian Lagoon and Memel - panoramio.jpg|thumb|[[Curonian Lagoon]], [[Curonian Spit|Spit]] and [[Klaipėda]]]]

An arm of the [[North Atlantic Ocean]], the Baltic Sea is enclosed by [[Sweden]] and [[Denmark]] to the west, [[Finland]] to the northeast, and the [[Baltic states|Baltic countries]] to the southeast.

It is about {{convert|1600|km|abbr=on}} long, an average of {{convert|193|km|abbr=on}} wide, and an average of {{convert|55|m|ft}} deep. The maximum depth is {{convert|459|m|ft|abbr=on}} which is on the Swedish side of the center. The surface area is about {{convert|349644|km2|abbr=on}} <ref>{{cite web|title=EuroOcean |url=http://www.eurocean.org/np4/323.html |access-date=14 April 2014 |url-status=dead |archive-url=https://web.archive.org/web/20140415124200/http://www.eurocean.org/np4/323.html |archive-date=15 April 2014}}</ref> and the volume is about {{convert|20000|km3|abbr=on}}. The periphery amounts to about {{convert|8000|km|abbr=on}} of coastline.<ref>{{cite web|url=http://www.envir.ee/baltics/geograph.htm |title=Geography of the Baltic Sea Area |access-date=27 August 2005 |url-status=dead |archive-url=https://web.archive.org/web/20060421230004/http://www.envir.ee/baltics/geograph.htm |archive-date=21 April 2006 }} at envir.ee. (archived) (21 April 2006). Retrieved on 23 June 2011.</ref>

The Baltic Sea is one of the largest [[brackish water|brackish]] inland seas by area, and occupies a basin (a ''[[Zungenbecken]]'') formed by glacial erosion during the last few [[ice age]]s.

{| class="wikitable sortable"
|+Physical characteristics of the Baltic Sea, its main sub-regions, and the transition zone to the Skagerrak/North Sea area<ref>{{Cite web |url=http://www.helcom.fi/Lists/Publications/BSEP104.pdf |title=p. 7 |access-date=27 November 2015 |archive-date=8 December 2015 |archive-url=https://web.archive.org/web/20151208055840/http://www.helcom.fi/Lists/Publications/BSEP104.pdf |url-status=live }}</ref>
! style="background: DarkCyan; color: white; text-align: center" rowspan=2| Sub-area
! style="background: DarkCyan; color: white; text-align: center" colspan=2| Area
! style="background: DarkCyan; color: white; text-align: center" colspan=2| Volume
! style="background: DarkCyan; color: white; text-align: center" colspan=2| Maximum depth
! style="background: DarkCyan; color: white; text-align: center" colspan=2| Average depth
|-
! style="background: DarkCyan; color: white; text-align: center"| km<sup>2</sup>
! style="background: DarkCyan; color: white; text-align: center"| sq mi
! style="background: DarkCyan; color: white; text-align: center"| km<sup>3</sup>
! style="background: DarkCyan; color: white; text-align: center"| cu mi
! style="background: DarkCyan; color: white; text-align: center"| m
! style="background: DarkCyan; color: white; text-align: center"| ft
! style="background: DarkCyan; color: white; text-align: center"| m
! style="background: DarkCyan; color: white; text-align: center"| ft
|-
| style="text-align: left"|Baltic proper
|{{convert|211,069|km2|sqmi|disp=table|sortable=on}}
|{{convert|13,045|km3|cumi|disp=table|sortable=on}}
|{{convert|459|m|ft|disp=table|sortable=on}}
|{{convert|62.1|m|ft|disp=table|sortable=on}}
|-
| style="text-align: left"|Gulf of Bothnia
|{{convert|115,516|km2|sqmi|disp=table|sortable=on}}
|{{convert|6,389|km3|cumi|disp=table|sortable=on}}
|{{convert|230|m|ft|disp=table|sortable=on}}
|{{convert|60.2|m|ft|disp=table|sortable=on}}
|-
| style="text-align: left"|Gulf of Finland
|{{convert|29,600|km2|sqmi|disp=table|sortable=on}}
|{{convert|1,100|km3|cumi|disp=table|sortable=on}}
|{{convert|123|m|ft|disp=table|sortable=on}}
|{{convert|38.0|m|ft|disp=table|sortable=on}}
|-
| style="text-align: left"|Gulf of Riga
|{{convert|16,300|km2|sqmi|disp=table|sortable=on}}
|{{convert|424|km3|cumi|disp=table|sortable=on}}
|{{convert|60|m|ft|disp=table|sortable=on}}
|{{convert|26.0|m|ft|disp=table|sortable=on}}
|-
| style="text-align: left"| Belt Sea/Kattegat
|{{convert|42,408|km2|sqmi|disp=table|sortable=on}}
|{{convert|802|km3|cumi|disp=table|sortable=on}}
|{{convert|109|m|ft|disp=table|sortable=on}}
|{{convert|18.9|m|ft|disp=table|sortable=on}}
|-
! style="text-align: left"| Total Baltic Sea
!{{convert|415,266|km2|sqmi|disp=table|sortable=on}}
!{{convert|21,721|km3|cumi|disp=table|sortable=on}}
!{{convert|459|m|ft|disp=table|sortable=on}}
!{{convert|52.3|m|ft|disp=table|sortable=on}}
|}

=== Extent ===
The [[International Hydrographic Organization]] defines the limits of the Baltic Sea as follows:<ref>{{cite web|url=https://iho.int/uploads/user/pubs/standards/s-23/S-23_Ed3_1953_EN.pdf |title=Limits of Oceans and Seas, 3rd edition |year=1953 |publisher=International Hydrographic Organization |access-date=28 December 2020 |archive-url=https://web.archive.org/web/20111008191433/http://www.iho-ohi.net/iho_pubs/standard/S-23/S23_1953.pdf |archive-date=8 October 2011 }}</ref>

:Bordered by the coasts of Germany, Denmark, Poland, Sweden, Finland, Russia, Estonia, Latvia, and Lithuania, it extends north-eastward of the following limits:
:*''In the [[Little Belt]].'' A line joining [[Nieby|Falshöft]] ({{coord|54|47|N|9|57.5|E|display=inline}}) and Vejsnæs Nakke ([[Ærø]]: {{coord|54|49|N|10|26|E|display=inline}}).
:*''In the [[Great Belt]].'' A line joining Gulstav (South extreme of [[Langeland]] Island) and Kappel Kirke ({{coord|54|46|N|11|01|E|display=inline}}) on Island of [[Lolland]].
:*''In the [[Guldborgsund|Guldborg Sound]].'' A line joining Flinthorne-Rev and Skjelby ({{coord|54|38|N|11|53|E|display=inline}}).
:*''In [[Øresund|the Sound]].'' A line joining [[Stevns Peninsula|Stevns]] Lighthouse ({{coord|55|17|N|12|27|E|display=inline}}) and [[Falsterbo|Falsterbo Point]] ({{coord|55|23|N|12|49|E|display=inline}}).

=== Subdivisions ===
[[File:Baltic marine subdivisions and drainage basins.gif|thumb|Regions and basins of the Baltic Sea:<ref>{{cite web|url=http://www.baltic.vtt.fi/demo/baltmap.htm|title=Baltic Sea area clickable map|website=www.baltic.vtt.fi|access-date=11 April 2008|archive-url=https://web.archive.org/web/20071023052150/http://www.baltic.vtt.fi/demo/baltmap.htm|archive-date=23 October 2007|url-status=dead}}</ref><br />1 = [[Bothnian Bay]]<br />2 = [[Bothnian Sea]]<br />1 + 2 = [[Gulf of Bothnia]], partly also 3 & 4<br />3 = [[Archipelago Sea]]<br />4 = [[Åland Sea]]<br />5 = [[Gulf of Finland]]<br />6 = Northern Baltic Proper<br />7 = Western [[Gotland Basin]]<br />8 = Eastern [[Gotland Basin]]<br />9 = [[Gulf of Riga]]<br />10 = [[Bay of Gdańsk]]/Gdansk Basin<br />11 = [[Bornholm]] Basin and [[Hanöbukten|Hanö Bight]]<br />12 = [[Cape Arkona|Arkona]] Basin<br />6–12 = [[Baltic Proper]]<br />13 = [[Kattegat]], not an integral part of the Baltic Sea<br />14 = Belt Sea ([[Little Belt]] and [[Great Belt]])<br />15 = [[Öresund]] (The Sound)<br />14 + 15 = [[Danish straits]], not an integral part of the Baltic Sea]]

The northern part of the Baltic Sea is known as the [[Gulf of Bothnia]], of which the northernmost part is the Bay of Bothnia <!-- redirects to: --> or [[Bothnian Bay]]. The more rounded southern basin of the gulf is called [[Bothnian Sea]] and immediately to the south of it lies the [[Sea of Åland]]. The [[Gulf of Finland]] connects the Baltic Sea with [[Saint Petersburg]]. The [[Gulf of Riga]] lies between the [[Latvia]]n capital city of [[Riga]] and the [[Estonia]]n island of [[Saaremaa]].

The Northern Baltic Sea lies between the [[Stockholm]] area, southwestern Finland, and Estonia. The [[Gotland Basin|Western and Eastern Gotland basins]] form the major parts of the Central Baltic Sea or Baltic proper. The [[Bornholm]] Basin is the area east of Bornholm, and the shallower [[Cape Arkona|Arkona]] Basin extends from Bornholm to the Danish isles of [[Falster]] and [[Zealand (Denmark)|Zealand]].

In the south, the [[Bay of Gdańsk]] lies east of the [[Hel Peninsula]] on the Polish coast and west of the [[Sambia Peninsula]] in [[Kaliningrad Oblast]]. The [[Bay of Pomerania]] lies north of the islands of [[Usedom|Usedom/Uznam]] and [[Wolin]], east of [[Rügen]]. Between Falster and the German coast lie the [[Bay of Mecklenburg]] and [[Bay of Lübeck]]. The westernmost part of the Baltic Sea is the [[Bay of Kiel]]. The three [[Danish straits]], the [[Great Belt]], the [[Little Belt]] and [[Öresund|The Sound]] (''Öresund''/''Øresund''), connect the Baltic Sea with the [[Kattegat]] and [[Skagerrak]] strait in the [[North Sea]].

===Temperature and ice===
[[File:BalticSea March2000 NASA-S2000084115409.png|thumb|Satellite image of the Baltic Sea in a mild winter]]
[[File:Baltic Sea 1551 (5496745361).jpg|thumb|Traversing Baltic Sea and ice]]
[[File:Skiing on the ice in Haukilahti.jpg|thumb|On particularly cold winters, the coastal parts of the Baltic Sea freeze into ice thick enough to walk or ski on.]]
The water temperature of the Baltic Sea varies significantly depending on exact location, season and depth. At the Bornholm Basin, which is located directly east of the island of the same name, the surface temperature typically falls to {{convert|0-5|C|F|abbr=on}} during the peak of the winter and rises to {{convert|15-20|C|F|abbr=on}} during the peak of the summer, with an annual average of around {{convert|9-10|C|F|abbr=on}}.<ref name=OurBalticSea>{{cite web | url=http://stateofthebalticsea.helcom.fi/in-brief/our-baltic-sea/ | title=Our Baltic Sea | publisher=HELCOM | access-date=27 July 2018 | archive-date=26 July 2018 | archive-url=https://web.archive.org/web/20180726025617/http://stateofthebalticsea.helcom.fi/in-brief/our-baltic-sea/ | url-status=live }}</ref> A similar pattern can be seen in the [[Gotland Basin]], which is located between the island of Gotland and Latvia. In the deep of these basins the temperature variations are smaller. At the bottom of the Bornholm Basin, deeper than {{convert|80|m|ft|abbr=on}}, the temperature typically is {{convert|1-10|C|F|abbr=on}}, and at the bottom of the Gotland Basin, at depths greater than {{convert|225|m|ft|abbr=on}}, the temperature typically is {{convert|4-7|C|F|abbr=on}}.<ref name=OurBalticSea/> Generally, offshore locations, lower latitudes and islands maintain [[oceanic climate|maritime climate]]s, but adjacent to the water [[humid continental climate|continental climate]]s are common, especially on the [[Gulf of Finland]]. In the northern tributaries the climates transition from moderate continental to [[subarctic climate|subarctic]] on the northernmost coastlines.

On the long-term average, the Baltic Sea is ice-covered at the annual maximum for about 45% of its surface area. The ice-covered area during such a typical winter includes the [[Gulf of Bothnia]], the [[Gulf of Finland]], the [[Gulf of Riga]], the archipelago west of Estonia, the [[Stockholm archipelago]], and the [[Archipelago Sea]] southwest of Finland. The remainder of the Baltic does not freeze during a normal winter, except sheltered bays and shallow lagoons such as the [[Curonian Lagoon]]. The ice reaches its maximum extent in February or March; typical ice thickness in the northernmost areas in the [[Bothnian Bay]], the northern basin of the Gulf of Bothnia, is about {{convert|70|cm|0|abbr=on}} for landfast sea ice. The thickness decreases farther south.

Freezing begins in the northern extremities of the Gulf of Bothnia typically in the middle of November, reaching the open waters of the Bothnian Bay in early January. The [[Bothnian Sea]], the basin south of [[Kvarken]], freezes on average in late February. The Gulf of Finland and the Gulf of Riga freeze typically in late January. In 2011, the Gulf of Finland was completely frozen on 15 February.<ref>''[[Helsingin Sanomat]]'', 16 February 2011, p. A8.</ref>

The ice extent depends on whether the winter is mild, moderate, or severe. In severe winters ice can form around southern [[Sweden]] and even in the [[Danish straits]]. According to the 18th-century natural historian [[William Derham]], during the severe winters of 1703 and 1708, the ice cover reached as far as the Danish straits.<ref>Derham, William ''Physico-Theology: Or, A Demonstration of the Being and Attributes of God from His Works of Creation'' (London, 1713).</ref> Frequently, parts of the Gulf of Bothnia and the Gulf of Finland are frozen, in addition to coastal fringes in more southerly locations such as the Gulf of Riga. This description meant that the whole of the Baltic Sea was covered with ice.

Since 1720, the Baltic Sea has frozen over entirely 20 times, most recently in early 1987, which was the most severe winter in Scandinavia since 1720. The ice then covered {{convert|400000|km2|abbr=on}}. During the winter of 2010–11, which was quite severe compared to those of the last decades, the maximum ice cover was {{convert|315000|km2|abbr=on}}, which was reached on 25 February 2011. The ice then extended from the north down to the northern tip of [[Gotland]], with small ice-free areas on either side, and the east coast of the Baltic Sea was covered by an ice sheet about {{convert|25|to|100|km|0|abbr=on}} wide all the way to [[Gdańsk]]. This was brought about by a stagnant [[high-pressure area]] that lingered over central and northern Scandinavia from around 10 to 24 February. After this, strong southern winds pushed the ice further into the north, and much of the waters north of Gotland were again free of ice, which had then packed against the shores of southern Finland.<ref>''[[Helsingin Sanomat]]'', 10 February 2011, p. A4; 25 February 2011, p. A5; 11 June 2011, p. A12.</ref> The effects of the aforementioned high-pressure area did not reach the southern parts of the Baltic Sea, and thus the entire sea did not freeze over. However, floating ice was additionally observed near [[Świnoujście]] harbor in January 2010.

In recent years before 2011, the Bothnian Bay and the Bothnian Sea were frozen with solid ice near the Baltic coast and dense floating ice far from it. In 2008, almost no ice formed except for a short period in March.<ref>[http://www.ssec.wisc.edu/ Sea Ice Survey] {{Webarchive|url=https://web.archive.org/web/20161125040216/http://www.ssec.wisc.edu/ |date=25 November 2016 }} Space Science and Engineering Center, University of Wisconsin.</ref>

[[File:Jäämäed Puhtulaiul 1.JPG|thumb|Piles of drift ice on the shore of Puhtulaid, near [[Virtsu]], Estonia, in late April]]
During winter, [[fast ice]], which is attached to the shoreline, develops first, rendering ports unusable without the services of [[icebreaker]]s. [[Level ice]], [[ice sludge]], [[pancake ice]], and [[rafter ice]] form in the more open regions. The gleaming expanse of ice is similar to the [[Arctic]], with wind-driven pack ice and ridges up to {{convert|15|m|abbr=on}}. Offshore of the landfast ice, the ice remains very dynamic all year, and it is relatively easily moved around by winds and therefore forms [[pack ice]], made up of large piles and ridges pushed against the landfast ice and shores.

In spring, the Gulf of Finland and the Gulf of Bothnia normally thaw in late April, with some ice ridges persisting until May in the eastern extremities of the Gulf of Finland. In the northernmost reaches of the Bothnian Bay, ice usually stays until late May; by early June it is practically always gone. However, in the famine year of [[Famine of 1866-68|1867]] remnants of ice were observed as late as 17 July near [[Uddskär]].<ref>{{cite web|title=Nödåret 1867|url=http://byar.lulea.se/scripts/historia_visa.asp?By=79&No=114|archive-url=https://web.archive.org/web/20110727130208/http://byar.lulea.se/scripts/historia_visa.asp?By=79&No=114|url-status=dead|archive-date=27 July 2011|publisher=Byar i Luleå}}</ref> Even as far south as [[Øresund]], remnants of ice have been observed in May on several occasions; near [[Taarbaek]] on 15 May 1942 and near Copenhagen on 11 May 1771. Drift ice was also observed on 11 May 1799.<ref>{{cite web|title=Isvintrene i 40'erne|date=19 January 2008|url=http://vejr.tv2.dk/artikel/id-10070756%3Aisvintrene-i-40erne.html/mraid.js|publisher=TV 2|access-date=6 January 2017|archive-date=6 January 2017|archive-url=https://web.archive.org/web/20170106105613/http://vejr.tv2.dk/artikel/id-10070756%3Aisvintrene-i-40erne.html/mraid.js|url-status=live}}</ref><ref>{{cite web|url=http://natmus.dk/historisk-viden/temaer/militaerhistorie/soeofficeren-peter-schioennings-liv/kilder/peter-schioennings-dagbog/1771/|title=1771 – Nationalmuseet|access-date=15 April 2017|archive-url=https://web.archive.org/web/20170416044935/http://natmus.dk/historisk-viden/temaer/militaerhistorie/soeofficeren-peter-schioennings-liv/kilder/peter-schioennings-dagbog/1771/|archive-date=16 April 2017|url-status=dead}}</ref><ref>{{cite web|title=Is i de danske farvande i 1700-tallet|url=https://natmus.dk/historisk-viden/temaer/klima-i-historien/den-lille-istid-og-industrialiseringen/is-i-de-danske-farvande/|publisher=Nationalmuseet|access-date=18 February 2018|archive-date=18 February 2018|archive-url=https://web.archive.org/web/20180218091529/https://natmus.dk/historisk-viden/temaer/klima-i-historien/den-lille-istid-og-industrialiseringen/is-i-de-danske-farvande/|url-status=live}}</ref>

The ice cover is the main habitat for two large mammals, the [[grey seal]] (''Halichoerus grypus'') and the Baltic [[ringed seal]] (''Pusa hispida botnica''), both of which feed underneath the ice and breed on its surface. Of these two seals, only the Baltic ringed seal suffers when there is not adequate ice in the Baltic Sea, as it feeds its young only while on ice. The grey seal is adapted to reproducing also with no ice in the sea. The sea ice also harbors several species of algae that live in the bottom and inside unfrozen brine pockets in the ice.

Due to the often fluctuating winter temperatures between above and below freezing, the saltwater ice of the Baltic Sea can be treacherous and hazardous to walk on, in particular in comparison to the more stable fresh water-ice sheets in the interior lakes.

===Hydrography===
[[File:Ostseetiefen.png|thumb|Depths of the Baltic Sea in meters]]
The Baltic Sea flows out through the [[Danish straits]]; however, the flow is complex. A surface layer of brackish water discharges {{convert|940|km3|abbr=on}} per year into the [[North Sea]]. Due to the difference in [[salinity]], by salinity permeation principle, a sub-surface layer of more saline water moving in the opposite direction brings in {{convert|475|km3|abbr=on}} per year. It mixes very slowly with the upper waters, resulting in a salinity gradient from top to bottom, with most of the saltwater remaining below {{convert|40|to|70|m|abbr=on}} deep. The general circulation is anti-clockwise: northwards along its eastern boundary, and south along with the western one .<ref name=Alhonen>Alhonen, p. 88</ref>

The difference between the outflow and the inflow comes entirely from fresh [[water]]. More than 250 streams drain a basin of about {{convert|1600000|km2|abbr=on}}, contributing a volume of {{convert|660|km3|abbr=on}} per year to the Baltic. They include the major rivers of north Europe, such as the [[Oder]], the [[Vistula]], the [[Neman River|Neman]], the [[Daugava River|Daugava]] and the [[Neva]]. Additional fresh water comes from the difference of [[precipitation (meteorology)|precipitation]] less evaporation, which is positive.

An important source of salty water is infrequent inflows (also known as [[Major Baltic Inflow|major Baltic inflows]] or MBIs) of [[North Sea]] water into the Baltic. Such inflows, important to the Baltic ecosystem because of the oxygen they transport into the Baltic deeps, happen on average once per year, but large pulses that can replace the anoxic deep water in the [[Gotland Basin|Gotland Deep]] occur about once in ten years. Previously, it was believed that the frequency of MBIs had declined since 1980, but recent studies have challenged this view and no longer display a clear change in the frequency or intensity of saline inflows. Instead, a decadal variability in the intensities of MBIs is observed with a main period of approximately 30 years.<ref>{{Cite journal |last=Mohrholz |first=Volker |date=2018 |title=Major Baltic Inflow Statistics – Revised |journal=Frontiers in Marine Science |volume=5 |page=384 |doi=10.3389/fmars.2018.00384 |issn=2296-7745 |doi-access=free |bibcode=2018FrMaS...5..384M }}</ref><ref>{{Cite journal |last1=Lehmann |first1=Andreas |last2=Myrberg |first2=Kai |last3=Post |first3=Piia |last4=Chubarenko |first4=Irina |last5=Dailidiene |first5=Inga |last6=Hinrichsen |first6=Hans-Harald |last7=Hüssy |first7=Karin |last8=Liblik |first8=Taavi |last9=Meier |first9=H. E. Markus |last10=Lips |first10=Urmas |last11=Bukanova |first11=Tatiana |date=16 February 2022 |title=Salinity dynamics of the Baltic Sea |url=https://esd.copernicus.org/articles/13/373/2022/ |journal=Earth System Dynamics |language=English |volume=13 |issue=1 |pages=373–392 |doi=10.5194/esd-13-373-2022 |bibcode=2022ESD....13..373L |issn=2190-4979 |access-date=24 July 2023 |archive-date=21 July 2023 |archive-url=https://web.archive.org/web/20230721123134/https://esd.copernicus.org/articles/13/373/2022/ |url-status=live |doi-access=free }}</ref>

The water level is generally far more dependent on the regional wind situation than on tidal effects. However, tidal currents occur in narrow passages in the western parts of the Baltic Sea. Tides can reach {{convert|17 to 19|cm|in|1|abbr=on}} in the Gulf of Finland.<ref>{{Cite journal|last1=Medvedev|first1=I. P.|last2=Rabinovich|first2=A. B.|last3=Kulikov|first3=E. A.|date=September 2013|title=Tidal oscillations in the Baltic Sea|url=http://link.springer.com/10.1134/S0001437013050123|journal=Oceanology|language=en|volume=53|issue=5|pages=526–538|doi=10.1134/S0001437013050123|bibcode=2013Ocgy...53..526M|s2cid=129778127|issn=0001-4370|access-date=27 September 2021|archive-date=4 December 2022|archive-url=https://web.archive.org/web/20221204034253/https://link.springer.com/article/10.1134/S0001437013050123|url-status=live|url-access=subscription}}</ref>

The [[significant wave height]] is generally much lower than that of the [[North Sea]]. Quite violent, sudden storms sweep the surface ten or more times a year, due to large transient temperature differences and a long reach of the wind. Seasonal winds also cause small changes in sea level, of the order of {{convert|0.5|m|abbr=on}} .<ref name=Alhonen/> According to the media, during a storm in January 2017, an extreme wave above {{convert|14|m|ft|0|abbr=on}} has been measured and significant wave height of around {{convert|8|m|ft|0|abbr=on}} has been measured by the [[Finnish Meteorological Institute|FMI]]. A numerical study has shown the presence of events with {{convert|8 to 10|m|ft|0|abbr=on}} significant wave heights. Those extreme waves events can play an important role in the coastal zone on erosion and sea dynamics.<ref>{{Cite journal|last1=Rutgersson|first1=Anna|last2=Kjellström|first2=Erik|last3=Haapala|first3=Jari|last4=Stendel|first4=Martin|last5=Danilovich|first5=Irina|last6=Drews|first6=Martin|last7=Jylhä|first7=Kirsti|last8=Kujala|first8=Pentti|last9=Guo Larsén|first9=Xiaoli|last10=Halsnæs|first10=Kirsten|last11=Lehtonen|first11=Ilari|date=6 April 2021|title=Natural Hazards and Extreme Events in the Baltic Sea region|url=https://esd.copernicus.org/preprints/esd-2021-13/|journal=Earth System Dynamics Discussions|volume=13|issue=1|language=English|pages=251–301|doi=10.5194/esd-2021-13|s2cid=233556209|issn=2190-4979|doi-access=free|access-date=29 September 2021|archive-date=29 September 2021|archive-url=https://web.archive.org/web/20210929141707/https://esd.copernicus.org/preprints/esd-2021-13/|url-status=live}}</ref>

===Salinity===
[[File:Sunny day on the coast on Baltic sea.jpg|thumb|Baltic Sea near [[Klaipėda]] ([[Karklė]]).]]

The Baltic Sea is the world's largest [[brackish]] sea.<ref name=Leijonmalm2017>{{cite book | author1=Snoeijs-Leijonmalm P. | author2=E.Andrén | year=2017 | chapter=Why is the Baltic Sea so special to live in? | editor1=P. Snoeijs-Leijonmalm | editor2=H. Schubert | editor3=T. Radziejewska | title=Biological Oceanography of the Baltic Sea | publisher=Springer, Dordrecht | pages=23–84 | isbn=978-94-007-0667-5 }}</ref> Only two [[List of brackish bodies of water|other brackish waters]] are larger according to some measurements: The [[Black Sea]] is larger in both surface area and water volume, but most of it is located outside the [[continental shelf]] (only a small fraction is inland). The [[Caspian Sea]] is larger in water volume, but—despite its name—it is a lake rather than a sea.<ref name=Leijonmalm2017/>

The Baltic Sea's [[salinity]] is much lower than that of ocean water (which averages 3.5%), as a result of abundant freshwater runoff from the surrounding land (rivers, streams and alike), combined with the shallowness of the sea itself; runoff contributes roughly one-fortieth its total volume per year, as the volume of the basin is about {{convert|21000|km3|abbr=on}} and yearly runoff is about {{convert|500|km3|abbr=on}}.{{citation needed|date=July 2018}}

The open surface waters of the Baltic Sea "proper" generally have a salinity of 0.3 to 0.9%, which is border-line [[freshwater]]. The flow of freshwater into the sea from approximately two hundred rivers and the introduction of salt from the southwest builds up a gradient of salinity in the Baltic Sea. The highest surface salinities, generally 0.7–0.9%, are in the southwestern most part of the Baltic, in the Arkona and Bornholm basins (the former located roughly between southeast [[Zealand]] and Bornholm, and the latter directly east of Bornholm). It gradually falls further east and north, reaching the lowest in the [[Bothnian Bay]] at around 0.3%.<ref name=Hydrogeography&Oxygen>{{cite web | author=Viktorsson, L. | date=16 April 2018 | url=http://www.helcom.fi/baltic-sea-trends/environment-fact-sheets/hydrography/hydrography-and-oxygen-in-the-deep-basins/ | title=Hydrogeography and oxygen in the deep basins | publisher=HELCOM | access-date=27 July 2018 | archive-date=27 July 2018 | archive-url=https://web.archive.org/web/20180727225916/http://www.helcom.fi/baltic-sea-trends/environment-fact-sheets/hydrography/hydrography-and-oxygen-in-the-deep-basins | url-status=live }}</ref> Drinking the surface water of the Baltic as a means of survival would actually hydrate the body instead of [[dehydration|dehydrating]], as is the case with ocean water.<ref group="note">A healthy serum concentration of sodium is around 0.8–0.85%, and healthy kidneys can concentrate salt in urine to at least 1.4%.</ref>{{citation needed|date=July 2018}}

As saltwater is denser than freshwater, the bottom of the Baltic Sea is saltier than the surface. This creates a vertical stratification of the water column, a [[halocline]], that represents a barrier to the exchange of [[oxygen]] and nutrients, and fosters completely separate maritime environments.<ref>{{cite web|url=http://www.ices.dk/projects/balticsea/baltic%20sea-rse%20thulin%20and%20andrusaitis.pdf |title=The Baltic Sea: Its Past, Present and Future |url-status=dead |archive-url=https://web.archive.org/web/20070606211738/http://www.ices.dk/projects/balticsea/baltic%20sea-rse%20thulin%20and%20andrusaitis.pdf |archive-date=6 June 2007 }} &nbsp;{{small|(352&nbsp;KB)}}, Jan Thulin and Andris Andrushaitis, Religion, Science and the Environment Symposium V on the Baltic Sea (2003).</ref> The difference between the bottom and surface salinities varies depending on location. Overall it follows the same southwest to east and north pattern as the surface. At the bottom of the Arkona Basin (equaling depths greater than {{convert|40|m|ft|abbr=on|disp=or}}) and Bornholm Basin (depths greater than {{convert|80|m|ft|abbr=on|disp=or}}) it is typically 1.4–1.8%. Further east and north the salinity at the bottom is consistently lower, being the lowest in Bothnian Bay (depths greater than {{convert|120|m|ft|abbr=on|disp=or}}) where it is slightly below 0.4%, or only marginally higher than the surface in the same region.<ref name=Hydrogeography&Oxygen/>

In contrast, the salinity of the [[Danish straits]], which connect the Baltic Sea and Kattegat, tends to be significantly higher, but with major variations from year to year. For example, the surface and bottom salinity in the [[Great Belt]] is typically around 2.0% and 2.8% respectively, which is only somewhat below that of the Kattegat.<ref name=Hydrogeography&Oxygen/> The water surplus caused by the continuous inflow of rivers and streams to the Baltic Sea means that there generally is a flow of brackish water out through the Danish straits to the Kattegat (and eventually the Atlantic).<ref name=Muus1999>{{cite book |author1=Muus, B. |author2=J.G. Nielsen |author3=P. Dahlstrom |author4=B. Nystrom |year=1999 |title=Sea Fish |publisher=Scandinavian Fishing Year Book |isbn=978-8790787004 }}</ref> Significant flows in the opposite direction, salt water from the Kattegat through the Danish straits to the Baltic Sea, are less regular and are known as [[Major Baltic Inflow|major Baltic inflows (MBIs)]].

=== Major tributaries ===
{{See also|List of rivers of the Baltic Sea}}
The rating of [[Discharge (hydrology)|mean discharges]] differs from the ranking of hydrological lengths (from the most distant source to the sea) and the rating of the nominal lengths. [[Göta älv]], a tributary of the [[Kattegat]], is not listed, as due to the northward upper low-salinity-flow in the sea, its water hardly reaches the Baltic proper:

{| class="wikitable sortable" style="padding:6px; spacing:6px;"
!rowspan=2| Name 
!colspan=2| Mean discharge
!colspan=2| Length 
!colspan=2| Basin area 
!rowspan=2| States sharing the basin 
!rowspan=2| Longest watercourse
|-
!{{nowrap|m<sup>3</sup>/s}}
!{{nowrap|cu ft/s}}
!km
!mi
!{{nowrap|km<sup>2</sup>}}
!{{nowrap|sq mi}}
|-
|[[Neva]] (nominal) ||{{convert|2500|m3/s|cuft/s|disp=table|sortable=on}} || {{convert|74|km|mi|disp=table|sortable=on}} ||{{convert|281,000|km2|sqmi|disp=table|sortable=on}} ||rowspan=2|[[Russia]], [[Finland]] (Ladoga-affluent [[Vuoksi]]) ||rowspan=2| [[Suna River|Suna]] ({{convert|280|km|abbr=on|disp=semicolon}}) → [[Lake Onega]] ({{convert|160|km|abbr=on|disp=semicolon}}) →<br />[[Svir River|Svir]] ({{convert|224|km|abbr=on|disp=semicolon}}) → [[Lake Ladoga]] ({{convert|122|km|abbr=on|disp=semicolon}}) → Neva
|-
|Neva (hydrological) || {{convert|2500|m3/s|cuft/s|disp=table|sortable=on}} ||{{convert|860|km|mi|disp=table|sortable=on}} || {{convert|281,000|km2|sqmi|disp=table|sortable=on}}
|-
| [[Vistula]] || {{convert|1080|m3/s|cuft/s|disp=table|sortable=on}} || {{convert|1047|km|mi|disp=table|sortable=on}} || {{convert|194,424|km2|sqmi|disp=table|sortable=on}} || [[Poland]], tributaries: [[Belarus]], [[Ukraine]], [[Slovakia]] || [[Bug (river)|Bug]] ({{convert|774|km|abbr=on|disp=semicolon}}) → [[Narew]] ({{convert|22|km|abbr=on|disp=semicolon}}) → Vistula ({{convert|156|km|abbr=on|disp=semicolon}}) total 1{{convert|204|km|abbr=on|disp=semicolon}}
|-
| [[Daugava River|Daugava]] || {{convert|678|m3/s|cuft/s|disp=table|sortable=on}} || {{convert|1020|km|mi|disp=table|sortable=on}} || {{convert|87,900|km2|sqmi|disp=table|sortable=on}} || [[Russia]] (source), [[Belarus]], [[Latvia]] ||
|-
| [[Neman River|Neman]] || {{convert|678|m3/s|cuft/s|disp=table|sortable=on}} || {{convert|937|km|mi|disp=table|sortable=on}} || {{convert|98,200|km2|sqmi|disp=table|sortable=on}} || [[Belarus]] (source), [[Lithuania]], [[Russia]] ||
|-
| [[Kemijoki]] (main river) ||{{convert|556|m3/s|cuft/s|disp=table|sortable=on}} || {{convert|550|km|mi|disp=table|sortable=on}} ||{{convert|51,127|km2|sqmi|disp=table|sortable=on}} ||rowspan=2| [[Finland]], [[Norway]] (source of [[Ounasjoki]]) ||rowspan=2| longer tributary [[Kitinen]]
|-
| Kemijoki (river system) || {{convert|556|m3/s|cuft/s|disp=table|sortable=on}} || {{convert|600|km|mi|disp=table|sortable=on}} || {{convert|51,127|km2|sqmi|disp=table|sortable=on}}
|-
| [[Oder]] || {{convert|540|m3/s|cuft/s|disp=table|sortable=on}} || {{convert|866|km|mi|disp=table|sortable=on}} || {{convert|118,861|km2|sqmi|disp=table|sortable=on}} || [[Czech Republic]] (source), [[Poland]], [[Germany]] ||[[Warta]] ({{convert|808|km|abbr=on|disp=semicolon}}) → Oder ({{convert|180|km|abbr=on|disp=semicolon}}) total: {{convert|928|km|abbr=on|disp=semicolon}}
|-
| [[Lule älv]] || {{convert|506|m3/s|cuft/s|disp=table|sortable=on}} || {{convert|461|km|mi|disp=table|sortable=on}} || {{convert|25,240|km2|sqmi|disp=table|sortable=on}} || [[Sweden]] ||
|-
| [[Narva River|Narva]] (nominal) ||{{convert|415|m3/s|cuft/s|disp=table|sortable=on}} || {{convert|77|km|mi|disp=table|sortable=on}} ||{{convert|56,200|km2|sqmi|disp=table|sortable=on}} ||rowspan=2| [[Russia]] (source of Velikaya), [[Estonia]] ||rowspan=2| [[Velikaya River|Velikaya]] ({{convert|430|km|abbr=on|disp=semicolon}}) → [[Lake Peipus]] ({{convert|145|km|abbr=on|disp=semicolon}}) → Narva
|-
| Narva (hydrological) ||{{convert|415|m3/s|cuft/s|disp=table|sortable=on}} || {{convert|652|km|mi|disp=table|sortable=on}} || {{convert|56,200|km2|sqmi|disp=table|sortable=on}}
|-
| [[Torne älv]] (nominal) ||{{convert|388|m3/s|cuft/s|disp=table|sortable=on}} || {{convert|520|km|mi|disp=table|sortable=on}} ||{{convert|40,131|km2|sqmi|disp=table|sortable=on}} ||rowspan=2| [[Norway]] (source), [[Sweden]], [[Finland]] ||rowspan=2| Válfojohka → Kamajåkka → Abiskojaure → [[Abiskojokk]]<br />(total {{convert|40|km|abbr=on|disp=semicolon}}) → [[Torneträsk]] ({{convert|70|km|abbr=on|disp=semicolon}}) → Torne älv
|-
| Torne älv (hydrological) || {{convert|388|m3/s|cuft/s|disp=table|sortable=on}} ||{{convert|630|km|mi|disp=table|sortable=on}} || {{convert|40,131|km2|sqmi|disp=table|sortable=on}}
|}

=== Islands and archipelagoes ===
{{main|List of islands in the Baltic Sea}}
[[File:Skerries which are part of the Åland Islands.jpg|thumb|[[skerry|Skerries]] form an integral and typical part of many of the [[archipelago]]s of the Baltic Sea, such as these in the archipelago of [[Åland]], [[Finland]].]]
[[File:Korsö Kroksö Sandön February 2013.jpg|thumb|[[Stockholm archipelago]]]]
[[File:Bornholm luftaufnahme.jpg|thumb|Aerial view of [[Bornholm]], Denmark]]
[[File:Cloud cumulonimbus at baltic sea(1).jpg|thumb|At [[Öland]], Sweden]]
* [[Åland]] ([[Finland]], [[autonomous entity|autonomous]])
* [[Archipelago Sea]] ([[Finland]])
** [[Pargas]]
** [[Nagu]]
** [[Korpo]]
** [[Houtskär]]
** [[Kustavi]]
** [[Kimito]]
* [[Blekinge archipelago]] ([[Sweden]])
* [[Bornholm]], including [[Christiansø]] ([[Denmark]])
* [[Falster]] ([[Denmark]])
* [[Gotland]] ([[Sweden]])
* [[Hailuoto]] ([[Finland]])
* [[Kotlin Island|Kotlin]] ([[Russia]])
* [[Lolland]] ([[Denmark]])
* [[Kvarken]] archipelago, including [[Valsörarna]] ([[Finland]])
* [[Møn]] ([[Denmark]])
* [[Öland]] ([[Sweden]])
* [[Rügen]] ([[Germany]])
* [[Stockholm archipelago]] ([[Sweden]])
** [[Värmdön]] ([[Sweden]])
* [[Usedom]] or Uznam (split between [[Germany]] and [[Poland]])
* [[West Estonian archipelago]] ([[Estonia]]):
** [[Hiiumaa]]
** [[Muhu]]
** [[Saaremaa]]
** [[Vormsi]]
* [[Wolin]] ([[Poland]])
* [[Zealand]] ([[Denmark]])

===Coastal countries===
[[File:Population density in the Baltic Sea catchment area.svg|thumb|Population density in the Baltic Sea catchment area]]

Countries that border the sea: Denmark, Estonia, Finland, Germany, Latvia, Lithuania, Poland, Russia, Sweden.

Countries lands in the outer [[drainage basin]]: Belarus, Czech Republic, Norway, Slovakia, Ukraine.

The Baltic Sea drainage basin is roughly four times the surface area of the sea itself. About 48% of the region is forested, with Sweden and Finland containing the majority of the forest, especially around the Gulfs of Bothnia and Finland.

About 20% of the land is used for agriculture and pasture, mainly in Poland and around the edge of the Baltic Proper, in Germany, Denmark, and Sweden. About 17% of the basin is unused open land with another 8% of wetlands. Most of the latter are in the Gulfs of Bothnia and Finland.

The rest of the land is heavily populated. About 85&nbsp;million people live in the Baltic drainage basin, 15&nbsp;million within {{convert|10|km|0|abbr=on}} of the coast and 29&nbsp;million within {{convert|50|km|0|abbr=on}} of the coast. Around 22&nbsp;million live in population centers of over 250,000. 90% of these are concentrated in the {{convert|10|km|0|abbr=on}} band around the coast. Of the nations containing all or part of the basin, Poland includes 45% of the 85&nbsp;million, Russia 12%, Sweden 10% and the others less than 6% each.<ref>{{Cite journal|last=Sweitzer|first=J|date=May 2019|title=Land Use and Population Density in the Baltic Sea Drainage Basin: A GIS Database|url=https://www.researchgate.net/publication/237511351|journal=Ambio|volume=25|pages=20|via=ResearchGate|access-date=11 July 2019|archive-date=30 May 2020|archive-url=https://web.archive.org/web/20200530150109/https://www.researchgate.net/publication/237511351_LAND_USE_AND_POPULATION_DENSITY_IN_THE_BALTIC_SEA_DRAINAGE_BASIN_A_GIS_DATABASE|url-status=live}}</ref>

==== Cities ====
{{Main|List of cities and towns around the Baltic Sea}}
[[File:Spb 06-2017 img01 Spit of Vasilievsky Island.jpg|thumb|[[Vasilyevsky Island]] in [[Saint Petersburg]], Russia]]
[[File:Stockholm 8721-B (9870833193).jpg|thumb|[[Stockholm]] in Sweden]]
[[File:Riga Petrikirche Blick vom Turm 8.JPG|thumb|[[Riga]] in Latvia]]
[[File:Paasitorni by the sea.jpg|thumb|[[Helsinki]] in Finland]]
[[File:Calle Dlugie Pobrzeze, Gdansk, Polonia, 2013-05-20, DD 07.jpg|thumb|[[Gdańsk]] in Poland]]
[[File:Таллин. - panoramio.jpg|thumb|[[Tallinn]] in Estonia]]
'''The biggest coastal cities (by population):'''
{{colbegin|colwidth=30em}}
* [[Saint Petersburg]] (Russia) 5,392,992 (metropolitan area 6,000,000)
* [[Stockholm]] (Sweden) 962,154 (metropolitan area 2,315,612)
* [[Helsinki]] (Finland) 665,558 (metropolitan area 1,559,558)
* [[Riga]] (Latvia) 614,618 (metropolitan area 1,070,00)
* [[Gdańsk]] (Poland) 462,700 ([[Tricity, Poland|metropolitan area]] 1,041,000)
* [[Tallinn]] (Estonia) 458,398 (metropolitan area 542,983)
* [[Kaliningrad]] (Russia) 431,500
* [[Szczecin]] (Poland) 413,600 (metropolitan area 778,000)
* [[Espoo]] (Finland) 306,792 (part of Helsinki metropolitan area)
* [[Gdynia]] (Poland) 255,600 ([[Tricity, Poland|metropolitan area]] 1,041,000)
* [[Kiel]] (Germany) 247,000<ref>[http://www.kiel.de/rathaus/statistik/statistische_berichte/statistische_kurzinformationen/2012/Kurzinfo_Nr._151_-_Amtliche_Einwohnerzahl_im_Dezember_2011.pdf Statistische Kurzinformation] {{webarchive|url=https://web.archive.org/web/20121111143033/http://www.kiel.de/rathaus/statistik/statistische_berichte/statistische_kurzinformationen/2012/Kurzinfo_Nr._151_-_Amtliche_Einwohnerzahl_im_Dezember_2011.pdf |date=11 November 2012 }} (in German). Landeshauptstadt Kiel. Amt für Kommunikation, Standortmarketing und Wirtschaftsfragen Abteilung Statistik. Retrieved on 11 October 2012.</ref>
* [[Lübeck]] (Germany) 216,100
* [[Rostock]] (Germany) 212,700
* [[Klaipėda]] (Lithuania) 194,400
* [[Oulu]] (Finland) 191,050
* [[Turku]] (Finland) 180,350
{{colend}}
'''Other important ports:'''
{{colbegin|colwidth=15em}}
* ''Estonia:''
** [[Pärnu]] 44,568
** [[Maardu]] 16,570
** [[Sillamäe]] 16,567
* ''Finland:''
** [[Pori]] 83,272
** [[Kotka]] 54,887
** [[Kokkola]] 46,809
** [[Port of Naantali]] 18,789
** [[Mariehamn]] 11,372
** [[Hanko, Finland|Hanko]] 9,270
* ''Germany:''
** [[Flensburg]] 94,000
** [[Stralsund]] 58,000
** [[Greifswald]] 55,000
** [[Wismar]] 44,000
** [[Eckernförde]] 22,000
** [[Neustadt in Holstein]] 16,000
** [[Wolgast]] 12,000
** [[Sassnitz]] 10,000
* ''Latvia:''
** [[Liepāja]] 85,000
** [[Ventspils]] 44,000
* ''Lithuania:''
** [[Palanga]] 17,000
* ''Poland:''
** [[Kołobrzeg]] 44,800
** [[Świnoujście]] 41,500
** [[Police, West Pomeranian Voivodeship|Police]] 34,284
** [[Władysławowo]] 15,000
** [[Darłowo]] 14,000
* ''Russia:''
** [[Vyborg]] 79,962
** [[Baltiysk]] 34,000
* ''Sweden:''
** [[Norrköping]] 144,932
** [[Gävle]] 103,619
** [[Trelleborg]] 30,818
** [[Karlshamn]] 19,000
** [[Oxelösund]] 11,000
{{colend}}

==Geology==
{{main|Geology of the Baltic Sea}}
{{multiple image
| align = right
| image1 = Baltic History 7500-BC.svg
| width1 = 250
| alt1 =
| caption1 = [[Ancylus Lake]] around 8700 years [[Before Present|BP]]. The relic of Scandinavian Glacier in white. The rivers [[Svea älv]] (Svea river) and [[Göta älv]] formed an outlet to the [[Atlantic Ocean|Atlantic]].
| image2 = Suomi jaakauden jalkeen.png
| width2 = 177
| alt2 =
| caption2 = Much of modern [[Finland]] is former seabed or archipelago: illustrated are sea levels immediately after the last ice age.
| footer =
}}
{{Evolution of the Baltic Sea}}
The Baltic Sea somewhat resembles a [[river]]bed, with two tributaries, the [[Gulf of Finland]] and [[Gulf of Bothnia]]. [[Geology|Geological]] surveys show that before the [[Pleistocene]], instead of the Baltic Sea, there was a wide plain around a great river that paleontologists call the [[Eridanos (geology)|Eridanos]]. Several Pleistocene [[glaciation|glacial]] episodes scooped out the river bed into the sea basin. By the time of the last, or [[Eemian Stage]] ([[Marine isotopic stage|MIS]]&nbsp;5e), the Eemian Sea was in place. Sometimes the Baltic Sea is considered a very large [[estuary]], with freshwater outflow from numerous rivers.<ref name="o502">{{cite journal | last1=Myrberg | first1=Kai | last2=Korpinen | first2=Samuli | last3=Uusitalo | first3=Laura | title=Physical oceanography sets the scene for the Marine Strategy Framework Directive implementation in the Baltic Sea | journal=Marine Policy | publisher=Elsevier BV | volume=107 | year=2019 | issn=0308-597X | doi=10.1016/j.marpol.2019.103591 | doi-access=free | page=103591| bibcode=2019MarPo.10703591M }}</ref>

From that time the waters underwent a geologic history summarized under the names listed below. Many of the stages are named after marine animals (e.g. the [[Littorina]] [[mollusk]]) that are clear markers of changing water temperatures and salinity.

The factors that determined the sea's characteristics were the submergence or emergence of the region due to the weight of ice and subsequent isostatic readjustment, and the connecting channels it found to the [[North Sea]]-[[Atlantic Ocean|Atlantic]], either through the straits of [[Denmark]] or at what are now the large lakes of [[Sweden]], and the [[White Sea]]-[[Arctic Sea]]. There are a number of named and dated stages in the evolution of the Baltic Sea:<ref>{{cite journal|last1=Rosentau|first1=A.|last2=Klemann|first2=V.|last3=Bennike|first3=O.|last4=Steffen|first4=H.|last5=Wehr|first5=J.|last6=Latinović|first6=M.|last7=Bagge|first7=M.|last8=Ojala|first8=A.|last9=Berglund|first9=M.|last10=Becher|first10=G.P.|last11=Schoning|first11=K.|year=2021|title=A Holocene relative sea-level database for the Baltic Sea|journal=Quaternary Science Reviews|volume =266|at=107071|doi=10.1016/j.quascirev.2021.107071|doi-access=free|bibcode=2021QSRv..26607071R }}</ref> 
* [[Eemian Sea]], about 130,000–115,000 years [[Before Present|BP]] 
* [[Baltic Ice Lake]], 16,000–11,700 years {{abbr|cal.|calibrated}} BP
* [[Yoldia Sea]], 11,700–10,700 years cal. BP
* [[Ancylus Lake]], 10,700–9,800 years cal. BP
* [[Mastogloia Sea]], 9,800–8,500 years cal. BP
* [[Littorina Sea]], 8,500–4,000 years cal. BP
* Post-Littorina Sea, 4,000–present

The land is still emerging [[isostasy|isostatically]] from its depressed state, which was caused by the weight of ice during the last glaciation. The phenomenon is known as [[post-glacial rebound]]. Consequently, the surface area and the depth of the sea are diminishing. The uplift is about eight millimeters per year on the Finnish coast of the northernmost Gulf of Bothnia. In the area, the former seabed is only gently sloping, leading to large areas of land being reclaimed in what are, geologically speaking, relatively short periods (decades and centuries).

===The "Baltic Sea anomaly"===
{{main|Baltic Sea anomaly}}
The "Baltic Sea anomaly" is a feature on an indistinct [[sonar]] image taken by Swedish salvage divers on the floor of the northern Baltic Sea in June 2011. The treasure hunters suggested the image showed an object with unusual features of seemingly extraordinary origin. Speculation published in [[Tabloid journalism|tabloid newspapers]] claimed that the object was a sunken [[UFO]]. A consensus of experts and scientists say that the image most likely shows a natural [[geological formation]].<ref name="Snopes">{{cite web|last1=Mikkelson|first1=David|title=UFO at the Bottom of the Baltic Sea? Rumor: Photograph shows a UFO discovered at the bottom of the Baltic Sea.|url=http://www.snopes.com/photos/supernatural/balticufo.asp|website=Urban Legends Reference Pages© 1995-2017 by Snopes.com|date=9 January 2015|publisher=Snopes.com|access-date=1 August 2017|archive-date=30 May 2020|archive-url=https://web.archive.org/web/20200530150111/https://www.snopes.com/fact-check/unidentified-submerged-object/|url-status=live}}</ref><ref name="HowStuffWorks">{{cite web|last1=Kershner|first1=Kate|title=What is the Baltic Sea anomaly?|url=http://science.howstuffworks.com/environmental/earth/oceanography/baltic-sea-anomaly.htm|website=How Stuff Works|date=7 April 2015|publisher=HowStuffWorks, a division of [[InfoSpace Holdings LLC.]]|access-date=1 August 2017|archive-date=12 October 2017|archive-url=https://web.archive.org/web/20171012154533/http://science.howstuffworks.com/environmental/earth/oceanography/baltic-sea-anomaly.htm|url-status=live}}</ref><ref name="LiveScience">{{cite web|last1=Wolchover|first1=Natalie|title=Mysterious' Baltic Sea Object Is a Glacial Deposit|url=https://www.livescience.com/22846-mysterious-baltic-sea-object-is-a-glacial-deposit.html|website=Live Science|date=30 August 2012|publisher=Live Science, Purch|access-date=1 August 2017|archive-date=2 August 2017|archive-url=https://web.archive.org/web/20170802043222/https://www.livescience.com/22846-mysterious-baltic-sea-object-is-a-glacial-deposit.html|url-status=live}}</ref><ref name=PopMech>{{cite journal|last=Main|first=Douglas|title=Underwater UFO? Get Real, Experts Say|journal=Popular Mechanics|date=2 January 2012|url=http://www.popularmechanics.com/technology/aviation/ufo/underwater-ufo-get-real-experts-say|access-date=14 March 2018|archive-date=28 December 2014|archive-url=https://web.archive.org/web/20141228221843/http://www.popularmechanics.com/technology/aviation/ufo/underwater-ufo-get-real-experts-say|url-status=live}}</ref><ref name=":0">Interview of Finnish planetary geomorphologist Jarmo Korteniemi (at 1:10:45) on {{Citation|last=Mars Moon Space Tv|title=Baltic Sea Anomaly. The Unsolved Mystery. Part 1-2|date=30 January 2017|url=https://www.youtube.com/watch?v=inIBLxONMBM&t=4245| archive-url=https://ghostarchive.org/varchive/youtube/20211123/inIBLxONMBM| archive-date=23 November 2021 | url-status=live|access-date=14 March 2018}}{{cbignore}}</ref>

== Biology ==
===Fauna and flora===
{{see also|List of fish in Sweden}}
The fauna of the Baltic Sea is a mixture of marine and freshwater species. Among marine fishes are [[Atlantic cod]], [[Atlantic herring]], [[European hake]], [[European plaice]], [[European flounder]], [[shorthorn sculpin]] and [[turbot]], and examples of freshwater species include [[European perch]], [[northern pike]], [[Coregonus|whitefish]] and [[common roach]]. Freshwater species may occur at outflows of rivers or streams in all coastal sections of the Baltic Sea. Otherwise, marine species dominate in most sections of the Baltic, at least as far north as [[Gävle]], where less than one-tenth are freshwater species. Further north the pattern is inverted. In the Bothnian Bay, roughly two-thirds of the species are freshwater. In the far north of this bay, saltwater species are almost entirely absent.<ref name=OurBalticSea/> For example, the [[common starfish]] and [[shore crab]], two species that are very widespread along European coasts, are both unable to cope with the significantly lower salinity. Their range limit is west of Bornholm, meaning that they are absent from the vast majority of the Baltic Sea.<ref name=OurBalticSea/> Some marine species, like the Atlantic cod and European flounder, can survive at relatively low salinities but need higher salinities to breed, which therefore occurs in deeper parts of the Baltic Sea.<ref name=Nissling1997>{{cite journal |author1=Nissling, L. |author2=A. Westin |year=1997 |title=Salinity requirements for successful spawning of Baltic and Belt Sea cod and the potential for cod stock interactions in the Baltic Sea |journal=Marine Ecology Progress Series |volume=152 |issue=1/3 |pages=261–271 |doi=10.3354/meps152261 |bibcode=1997MEPS..152..261N |doi-access=free }}</ref><ref name=Momigliano2018>{{cite journal |author1=Momigliano, M. |author2=G.P.J. Denys |author3=H. Jokinen |author4=J. Merilä |year=2018 |title=Platichthys solemdali sp. nov. (Actinopterygii, Pleuronectiformes): A New Flounder Species From the Baltic Sea |journal=Front. Mar. Sci. |volume=5 |issue=225 |doi=10.3389/fmars.2018.00225 |doi-access=free |bibcode=2018FrMaS...5..225M }}</ref> The common [[blue mussel]] is the dominating animal species, and makes up more than 90% of the total animal biomass in the sea.<ref>{{Cite book |url=https://books.google.com/books?id=VIopLSQyI5MC&dq=Baltic+Sea+blue+mussel+population+belt+living+filter&pg=PA164 |title=Environmental Science : Understanding, Protecting and Managing the Environment in the Baltic Sea Region |isbn=978-91-970017-0-0 |access-date=24 September 2023 |archive-date=15 October 2023 |archive-url=https://web.archive.org/web/20231015072451/https://books.google.com/books?id=VIopLSQyI5MC&dq=Baltic+Sea+blue+mussel+population+belt+living+filter&pg=PA164 |url-status=live |last1=Rydén |first1=Lars |last2=Migula |first2=Pawel |last3=Andersson |first3=Magnus |date=11 January 2024 |publisher=Baltic University Press }}</ref>

There is a decrease in species richness from the Danish belts to the [[Gulf of Bothnia]]. The decreasing salinity along this path causes restrictions in both physiology and habitats.<ref>{{cite book|title=Oceanography: An Illustrated Guide |editor-first=C. P. |editor-last=Summerhayes |editor2-first=S. A. |editor2-last=Thorpe |chapter=Life in Estuaries, Salt Marshes, Lagoons and Coastal Waters |first1=A. P. M. |last1=Lockwood |first2=M. |last2=Sheader |first3=J. A. |last3=Williams |edition=2nd |year=1998 |publisher=Manson Publishing |location=London |isbn=978-1-874545-37-8 |page=246}}</ref> At more than 600 species of invertebrates, fish, aquatic mammals, aquatic birds and [[macrophyte]]s, the Arkona Basin (roughly between southeast Zealand and Bornholm) is far richer than other more eastern and northern basins in the Baltic Sea, which all have less than 400 species from these groups, with the exception of the Gulf of Finland with more than 750 species. However, even the most diverse sections of the Baltic Sea have far fewer species than the almost-full saltwater Kattegat, which is home to more than 1600 species from these groups.<ref name=OurBalticSea/> The lack of [[tide]]s has affected the marine species as compared with the Atlantic.

Since the Baltic Sea is so young there are only two or three known [[Endemism|endemic]] species: the brown alga ''[[Fucus radicans]]'' and the flounder ''[[Platichthys solemdali]]''. Both appear to have evolved in the Baltic basin and were only recognized as species in 2005 and 2018 respectively, having formerly been confused with more widespread relatives.<ref name=Momigliano2018/><ref name=Pereyra2009>{{cite journal |author1=Pereyra, R.T. |author2=L. Bergström |author3= L. Kautsky |author4=K. Johannesson |year=2009 |title=Rapid speciation in a newly opened postglacial marine environment, the Baltic Sea |journal=BMC Evolutionary Biology |volume=9 |issue=70 |pages= 70|doi=10.1186/1471-2148-9-70 |pmid= 19335884|pmc= 2674422 |doi-access=free |bibcode=2009BMCEE...9...70P }}</ref> The tiny [[Parvicardium hauniense|Copenhagen cockle]] (''Parvicardium hauniense''), a rare mussel, is sometimes considered endemic, but has now been recorded in the Mediterranean.<ref>Red List Benthic Invertebrate Expert Group (2013) {{URL|http://www.helcom.fi/Red List Species Information Sheet/HELCOM Red List Parvicardium hauniense.pdf|Parvicardium hauniense}}. HELCOM. Accessed 27 July 2018.</ref> However, some consider non-Baltic records to be misidentifications of juvenile [[lagoon cockle]]s (''Cerastoderma glaucum'').<ref>{{cite web | publisher=National Museum Wales | date=17 May 2016 | title=Parvicardium hauniense | url=https://naturalhistory.museumwales.ac.uk/britishbivalves/browserecord.php?-recid=122 | access-date=27 July 2018 | archive-date=27 July 2018 | archive-url=https://web.archive.org/web/20180727181346/https://naturalhistory.museumwales.ac.uk/britishbivalves/browserecord.php?-recid=122 | url-status=live }}</ref> Several widespread marine species have distinctive subpopulations in the Baltic Sea adapted to the low salinity, such as the Baltic Sea forms of the Atlantic herring and [[Cyclopterus lumpus|lumpsucker]], which are smaller than the widespread forms in the North Atlantic.<ref name=Muus1999/>

A peculiar feature of the fauna is that it contains a number of glacial [[glacial relict|relict species]], isolated populations of arctic species which have remained in the Baltic Sea since the last [[glaciation]], such as the large isopod ''[[Saduria entomon]]'', the Baltic subspecies of [[ringed seal]], and the [[fourhorn sculpin]]. Some of these relicts are derived from [[glacial lake]]s, such as  ''[[Monoporeia affinis]]'', which is a main element in the [[benthos|benthic fauna]] of the low-salinity [[Bothnian Bay]].

[[Cetacean]]s in the Baltic Sea are monitored by the countries bordering the sea and data compiled by various intergovernmental bodies, such as [[ASCOBANS]]. A critically endangered population of [[harbor porpoise]] inhabit the Baltic proper, whereas the species is abundant in the outer Baltic (Western Baltic and [[Danish straits]]) and occasionally oceanic and out-of-range species such as [[minke whale]]s,<ref>[http://www.marlin.ac.uk/species/detail/1994 Minke whale (Balaenoptera acutorostrata)] {{Webarchive|url=https://web.archive.org/web/20161030203014/http://www.marlin.ac.uk/species/detail/1994 |date=30 October 2016 }} – MarLIN, The Marine Life Information Network</ref> [[bottlenose dolphin]]s,<ref>{{Cite web|url=http://www.thenews.pl/1/9/Artykul/217965,Baltic-dolphin-sightings-confirmed|title=Baltic dolphin sightings confirmed|access-date=18 November 2015|archive-date=31 March 2019|archive-url=https://web.archive.org/web/20190331171938/http://www.thenews.pl/1/9/Artykul/217965,Baltic-dolphin-sightings-confirmed|url-status=live}}</ref> [[beluga whale]]s,<ref>[https://www.rgo.ru/en/projects/protection-endangered-species-beluga-white-whale/about-beluga About the beluga] {{Webarchive|url=https://web.archive.org/web/20161031085206/https://www.rgo.ru/en/projects/protection-endangered-species-beluga-white-whale/about-beluga |date=31 October 2016 }} – Russian Geographical Society</ref> [[orca]]s,<ref>{{cite iucn |author=Reeves, R. |author2=Pitman, R.L. |author3=Ford, J.K.B. |date=2017 |title=''Orcinus orca'' |volume=2017 |page=e.T15421A50368125 |doi=10.2305/IUCN.UK.2017-3.RLTS.T15421A50368125.en |access-date=12 November 2021}}</ref> and [[beaked whale]]s<ref>{{Cite web|url=http://us.whales.org/news/2015/10/rare-sowerbys-beaked-whale-spotted-in-baltic-sea|title=Rare Sowerby's beaked whale spotted in the Baltic Sea|access-date=18 November 2015|archive-date=19 November 2015|archive-url=https://web.archive.org/web/20151119005206/http://us.whales.org/news/2015/10/rare-sowerbys-beaked-whale-spotted-in-baltic-sea|url-status=live}}</ref> visit the waters. In recent years, very small, but with increasing rates, [[fin whale]]s<ref>{{cite web|url=http://www.cetacea.de/news/archiv/2005/10/arch051001.shtml|title=Wieder Finnwal in der Ostsee|url-status=dead|archive-url=https://web.archive.org/web/20160415090735/http://www.cetacea.de/news/archiv/2005/10/arch051001.shtml|archive-date=15 April 2016}}</ref><ref>{{cite web|url=http://www.ostsee-zeitung.de/Region-Rostock/Rostock/Finnwal-in-der-Ostsee-gesichtet|title=Finnwal in der Ostsee gesichtet|first=Ostsee-Zeitung GmbH & Co.|last=KG|website=www.ostsee-zeitung.de|access-date=30 October 2016|archive-date=30 October 2016|archive-url=https://web.archive.org/web/20161030202908/http://www.ostsee-zeitung.de/Region-Rostock/Rostock/Finnwal-in-der-Ostsee-gesichtet|url-status=dead}}</ref><ref>{{cite web|url=http://www.augsburger-allgemeine.de/panorama/Angler-filmt-Wal-in-Ostsee-Bucht-id34821572.html|title=Angler filmt Wal in Ostsee-Bucht|first=Augsburger|last=Allgemeine|date=17 July 2015 |access-date=30 October 2016|archive-date=30 October 2016|archive-url=https://web.archive.org/web/20161030202039/http://www.augsburger-allgemeine.de/panorama/Angler-filmt-Wal-in-Ostsee-Bucht-id34821572.html|url-status=live}}</ref><ref>Jansson N.. 2007. [http://www.aftonbladet.se/nyheter/article11115075.ab "Vi såg valen i viken"] {{Webarchive|url=https://web.archive.org/web/20170907032600/http://www.aftonbladet.se/nyheter/article11115075.ab |date=7 September 2017 }}. [[Aftonbladet]]. Retrieved on 7 September 2017.</ref> and [[humpback whale]]s migrate into Baltic sea including mother and calf pair.<ref>{{Cite web|url=https://scienceinpoland.pap.pl/en/news/news%2C401331%2Cwhales-seen-again-in-the-waters-of-the-baltic-sea.html|title=Whales seen again in the waters of the Baltic Sea|website=Science in Poland|access-date=30 June 2022|archive-date=4 July 2022|archive-url=https://web.archive.org/web/20220704063444/https://scienceinpoland.pap.pl/en/news/news,401331,whales-seen-again-in-the-waters-of-the-baltic-sea.html|url-status=live}}</ref> Now extinct Atlantic [[grey whale]]s (remains found from [[Gräsö]] along [[Bothnian Sea]]/southern [[Bothnian Gulf]]<ref>Jones L.M..Swartz L.S.. Leatherwood S.. [https://books.google.com/books?id=GfGITi5NmJoC&dq=bothnia+whale&pg=PA41 The Gray Whale: Eschrichtius Robustus] {{Webarchive|url=https://web.archive.org/web/20221227075441/https://books.google.co.nz/books?id=GfGITi5NmJoC&pg=PA41&lpg=PA41&dq=bothnia+whale&source=bl&ots=7Y4sPhp6Ps&sig=maos19QFQH8mKODdOa59cQpV5hE&hl=en&sa=X&ved=0ahUKEwjT2veQ5YvWAhXEoZQKHfxfDiA4ChDoAQglMAA#v=onepage&q=bothnia%20whale&f=false |date=27 December 2022 }}. "Eastern Atlantic Specimens". pp. 41–44. [[Academic Press]]. Retrieved on 5 September 2017</ref> and [[Ystad]]<ref>[[Global Biodiversity Information Facility]]. [https://www.gbif.org/occurrence/1322462463 Occurrence Detail 1322462463] {{Webarchive|url=https://web.archive.org/web/20181106232818/https://www.gbif.org/occurrence/1322462463 |date=6 November 2018 }}. Retrieved on 21 September 2017</ref>) and eastern population of [[North Atlantic right whale]]s that is facing [[functional extinction]]<ref>{{Cite web|url=https://us.whales.org/whales-dolphins/species-guide/north-atlantic-right-whale/|title=North Atlantic right whale|first=George|last=Berry|access-date=16 June 2022|archive-date=25 May 2022|archive-url=https://web.archive.org/web/20220525034711/https://us.whales.org/whales-dolphins/species-guide/north-atlantic-right-whale/|url-status=live}}</ref> once migrated into Baltic Sea.<ref>{{cite web|url=http://www.fmap.ca/ramweb/media/biodiversity_loss/downloads/RegionalExtinctionExamples.pdf|archive-url=https://wayback.archive-it.org/0/20110425162323/http://www.fmap.ca//ramweb/media/biodiversity_loss/downloads/RegionalExtinctionExamples.pdf|url-status=dead|archive-date=25 April 2011|title=Regional Species Extinctions – Examples of regional species extinctions over the last 1000 years and more.}}</ref>

Other notable [[megafauna]] include the [[basking shark]]s.<ref>{{Cite web |url=http://deski.fi/download.php?file_name=BlnrYjTbXR.pdf |title=Archived copy |access-date=18 November 2015 |archive-date=7 August 2019 |archive-url=https://web.archive.org/web/20190807232618/http://deski.fi/download.php?file_name=BlnrYjTbXR.pdf |url-status=dead }}</ref>

===Environmental status===
{{further|Baltic Sea hypoxia}}
[[File:Baltic blooms ESA21514635.jpeg|thumb|Satellite photo of the Baltic Sea surrounding [[Gotland]], Sweden, with algae bloom (phytoplankton) swirling in the water]]
Satellite images taken in July 2010 revealed a massive [[algal bloom]] covering {{convert|377000|sqkm|mi2}} in the Baltic Sea. The area of the bloom extended from Germany and Poland to Finland. Researchers of the phenomenon have indicated that algal blooms have occurred every summer for decades. Fertilizer runoff from surrounding agricultural land has exacerbated the problem and led to increased [[eutrophication]].<ref>{{cite news|title=Satellite spies vast algal bloom in Baltic Sea|url=https://www.bbc.co.uk/news/science-environment-10740097|access-date=27 July 2010|newspaper=BBC News|date=23 July 2010| archive-url= https://web.archive.org/web/20100726191305/http://www.bbc.co.uk/news/science-environment-10740097| archive-date= 26 July 2010 | url-status= live}}</ref>

Approximately {{convert|100000|km2|0|abbr=on}} of the Baltic's seafloor (a quarter of its total area) is a variable [[Dead zone (ecology)|dead zone]]. The more saline (and therefore denser) water remains on the bottom, isolating it from surface waters and the atmosphere. This leads to decreased oxygen concentrations within the zone. It is mainly bacteria that grow in it, digesting organic material and releasing [[hydrogen sulfide]]. Because of this large anaerobic zone, the seafloor ecology differs from that of the neighboring Atlantic.

Plans to artificially oxygenate areas of the Baltic that have experienced eutrophication have been proposed by the [[University of Gothenburg]] and Inocean AB. The proposal intends to use wind-driven pumps to pump oxygen-rich surface water to a depth of around 130 m.<ref>{{cite web|title=Oxygenation at a Depth of 120 Meters Could Save the Baltic Sea, Researchers Demonstrate|url=https://www.sciencedaily.com/releases/2011/04/110418141617.htm|website=Science Daily|access-date=9 March 2018|archive-date=20 October 2017|archive-url=https://web.archive.org/web/20171020130835/https://www.sciencedaily.com/releases/2011/04/110418141617.htm|url-status=live}}</ref>

After [[World War II]], Germany had to be disarmed and large quantities of ammunition stockpiles were disposed directly into the Baltic Sea and the North Sea. Environmental experts and marine biologists warn that these ammunition dumps pose an environmental threat with potentially life-threatening consequences to the health and safety of humans on the coastlines of these seas.<ref>{{Cite web|url=https://www.dw.com/en/ticking-time-bombs-on-the-bottom-of-the-north-and-baltic-sea/a-40200208|title=Ticking time bombs on the bottom of the North and Baltic Sea|date=23 August 2017|website=DW.COM|language=en-GB|access-date=13 September 2019|archive-date=4 June 2020|archive-url=https://web.archive.org/web/20200604014153/https://www.dw.com/en/ticking-time-bombs-on-the-bottom-of-the-north-and-baltic-sea/a-40200208|url-status=live}}</ref>

== Future change ==

[[Climate change]], and [[Water pollution|pollution]] from agriculture and forestry, impose such strong effects on the ecosystems of the Baltic sea, that there is a concern the sea will turn from a [[carbon sink]] to a source of [[Carbon dioxide|CO2]] and [[methane]].<ref>{{cite web |last1=Korkman |first1=Anna |title=Warming Baltic Sea: a red flag for global oceans |url=https://phys.org/news/2024-07-baltic-sea-red-flag-global.html |website=Phys.org |access-date=19 July 2024}}</ref> Modelling climate change and the impact of well characterised factors such as post-glacial rebound before the year 2050, is complicated by the unique properties of the Baltic Sea area compared to say the adjacent North Sea and controversy as to the relative contributions of socio-economic factors such as land use to any warming component.<ref name="Meier2022">{{cite journal|last1=Meier|first1=H.M.|last2=Kniebusch, M.|last3=Dieterich, C.|last4=Gröger, M.|last5=Zorita, E.|last6=Elmgren, R.V|last7=Myrberg, K.|last8=Ahola, M.P.|last9=Bartosova, A.|last10=Bonsdorff, E.|last11=Börgel, F.|date=15 March 2022|title=Climate change in the Baltic Sea region: a summary|journal=Earth System Dynamics|volume=13|issue=1|pages=457–593|doi=10.5194/esd-13-457-2022|doi-access=free|bibcode=2022ESD....13..457M|hdl=11250/3043839|hdl-access=free}}</ref>{{rp|p=537}} These include its current brackish water, the southern subbasin tendency to have a vertical stratification of the halocline, and the northern subbasin seasonal sea ice cover.<ref name="Meier2022"/>{{rp|p=458}} [[Analytic confidence|High confidence]] future projections include: air temperature warming, more heavy precipitation episodes, less snow with less perifrost and glacial ice mass in northern catchment areas, more mild winters, raised mean water temperature with more marine heatwaves, intensified seasonal [[thermocline]]s without change in the [[thermohaline circulation]], and [[sea level rise]].<ref name="Meier2022"/>{{rp|pp=547, 458–9}} There are many more projections but these have lower confidence.<ref name="Meier2022"/>{{rp|pp=547, 458–9}}<ref group="note">All future projections have limits and make assumptions. The cause of the [[Younger Dryas]] which impacted on the Baltic area is unknown and such an event is not considered in most Baltic Sea future modelling.</ref>

== Economy ==
{{see also|Baltic Sea cruiseferries|Ports of the Baltic Sea|List of oil and gas fields of the Baltic Sea}}
[[File:Insel_Rügen-Strand_von_Sellin.jpg|thumb|Pedestrian pier in [[Sellin]], Germany]]
Construction of the [[Great Belt Bridge]] in Denmark (completed 1997) and the [[Øresund Bridge]]-Tunnel (completed 1999), linking Denmark with Sweden, provided a highway and railroad connection between Sweden and the Danish mainland (the [[Jutland Peninsula]], precisely the [[Zealand]]). The undersea tunnel of the Øresund Bridge-Tunnel provides for navigation of large ships into and out of the Baltic Sea. The Baltic Sea is the main trade route for the export of Russian petroleum. Countries neighboring the Baltic Sea have expressed concerns about this since a major oil leak in a seagoing tanker would be especially disastrous for the Baltic given the slow exchange of water in the ecosystem.<ref>{{Cite news |title=Shadow Fleet in Baltic Sea Poses Threat to Environment |url=https://www.bloomberg.com/graphics/2024-russia-shadow-oil-fleet-denmark-baltic-environment/ |archive-url=https://web.archive.org/web/20250205095159/https://www.bloomberg.com/graphics/2024-russia-shadow-oil-fleet-denmark-baltic-environment/ |archive-date=5 February 2025 |access-date=9 February 2025 |work=Bloomberg.com |language=en |url-status=live }}</ref><ref>{{Cite news |last=Wintour |first=Patrick |last2= |first2= |date=18 April 2024 |title='Russia doesn't care': Sweden sounds alarm over unsafe oil fleet |url=https://www.theguardian.com/world/2024/apr/18/swedish-foreign-minister-tobias-billstrom-unsafe-russian-oil-fleet-baltic-sea-environmental-catastrophe |access-date=9 February 2025 |work=The Guardian |language=en-GB |issn=0261-3077}}</ref><ref>{{Citation |last=Stigebrandt |first=A. |title=Physical Oceanography of the Baltic Sea |date=2001 |work=A Systems Analysis of the Baltic Sea |series=Ecological Studies |volume=148 |pages=19–74 |editor-last=Wulff |editor-first=Fredrik V. |url=https://link.springer.com/chapter/10.1007/978-3-662-04453-7_2 |access-date=9 February 2025 |place=Berlin, Heidelberg |publisher=Springer |language=en |doi=10.1007/978-3-662-04453-7_2 |isbn=978-3-662-04453-7 |editor2-last=Rahm |editor2-first=Lars A. |editor3-last=Larsson |editor3-first=Per|url-access=subscription }}</ref> The tourism industry surrounding the Baltic Sea is naturally concerned about [[oil pollution]].{{citation needed|date=April 2021}}

Much shipbuilding is carried out in the shipyards around the Baltic Sea. The largest shipyards are at [[Gdańsk]], [[Gdynia]], and [[Szczecin]], Poland; [[Kiel]], Germany; [[Karlskrona]] and [[Malmö]], Sweden; [[Rauma, Finland|Rauma]], [[Turku]], and [[Helsinki]], Finland; [[Riga]], [[Ventspils]], and [[Liepāja]], Latvia; [[Klaipėda]], Lithuania; and [[Saint Petersburg]], Russia.

Construction of the [[Fehmarn Belt Fixed Link]] between Denmark and Germany is due to finish in 2029. It will be a three-bore tunnel carrying four motorway lanes and two rail tracks.

Through the development of [[offshore wind power]] the Baltic Sea is expected to become a major source of energy for countries in the region. According to the Marienborg Declaration, signed in 2022, all EU Baltic Sea states have announced their intentions to have 19.6 gigawatts of offshore wind in operation by 2030.<ref>{{Cite news|url=https://www.euractiv.com/section/energy-environment/opinion/a-sea-of-change-energy-security-in-the-baltic-region/|title=A Sea of Change: Energy Security in the Baltic region|last=Trakimavicius|first=Lukas|work=EurActiv|access-date=26 July 2023|language=en-US|archive-date=26 July 2023|archive-url=https://web.archive.org/web/20230726112746/https://www.euractiv.com/section/energy-environment/opinion/a-sea-of-change-energy-security-in-the-baltic-region/|url-status=live}}</ref>

=== Ferries ===
There are several cargo and passenger ferries that operate on the Baltic Sea, such as

* Birka Gotland (cruises from Stockholm to Gotland and Åland Islands)
* [[Destination Gotland]] (Gotland-mainland Sweden)
* [[Eckerö Line]] (Estonia-Finland)
* [[Eckerö Linjen]] (Sweden-Åland Islands)
* [[Finnlines]] (Finland-Germany, Finland-Sweden, Germany-Sweden, Poland-Sweden)
* [[Polferries]] (Poland-Sweden, Poland-Denmark)
* [[Scandlines]] (Denmark-Germany)
* [[Stena Line]] (Denmark-Sweden, Germany-Sweden, Latvia-Sweden, Poland-Sweden) 
* [[Tallink]] and [[Silja Line|Tallink Silja]] (Estonia-Finland, Estonia-Sweden, Finland-Sweden)
* [[TT-Line]] (Germany-Lithuania, Germany-Sweden, Lithuania-Sweden, Poland-Sweden)
* [[Viking Line]] (Estonia-Finland, Finland-Sweden)
* [[Wasa Line|Wasaline]] (Finland-Sweden)

===Tourism===
[[File:View from Nida Lighthouse, Nida, Lithuania, 09-09-2023 05.jpg|thumb|[[Nida, Lithuania|Nida]] resort town in [[Klaipėda county]], Lithuania]]
[[File:Пляж в Светлогорске - panoramio.jpg|thumb|[[Svetlogorsk, Kaliningrad Oblast|Svetlogorsk]] resort town in [[Kaliningrad Oblast]], Russia]]
[[File:Mrzezyno east beach 2010-07 A.jpg|thumb|[[Mrzeżyno]] beach in Poland]]
{{col-begin|width=auto}}
{{col-break}}
'''Piers'''
* [[Ahlbeck (Usedom)]], Germany
* [[Bansin]], Germany
* [[Binz]], Germany
* [[Heiligendamm]], Germany
* [[Kühlungsborn]], Germany
* [[Sellin]], Germany
* [[Liepāja]], Latvia
* [[Šventoji, Lithuania]]
* [[Klaipėda]], Lithuania
* [[Gdańsk]], Poland
* [[Gdynia]], Poland
* [[Kołobrzeg]], Poland
* [[Międzyzdroje]], Poland
* [[Sopot]], Poland
{{col-break|gap=4em}}
'''Resort towns'''
* [[Haapsalu]], Estonia
* [[Kuressaare]], Estonia
* [[Narva-Jõesuu]], Estonia
* [[Pärnu]], Estonia
* [[Hanko, Finland|Hanko]], Finland
* [[Mariehamn]], Finland
* [[Binz]], Germany
* [[Heiligendamm]], Germany
* [[Heringsdorf]], Germany
* [[Travemünde]], Germany
* [[Sellin]], Germany
* [[Ueckermünde]], Germany
* [[Jūrmala]], Latvia
* [[Nida, Lithuania|Nida]], Lithuania
* [[Palanga]], Lithuania
* [[Šventoji, Lithuania]]
* [[Juodkrantė]], Lithuania
* [[Pervalka]], Lithuania
* [[Karklė]], Lithuania
* [[Kamień Pomorski]], Poland
* [[Kołobrzeg]], Poland
* [[Sopot]], Poland
* [[Świnoujście]], Poland
* [[Ustka]], Poland
* [[Svetlogorsk, Russia|Svetlogorsk]], Russia
{{col-end}}

== Critical Maritime Infrastructure (CMI) ==
Critical maritime infrastructure (CMI) includes pipelines, ports, undersea cables and energy installations.  Following a series of incidents between 2022 and 2025, critical infrastructure in the Baltic Sea has drawn growing political attention. In September 2022, both [[Nord Stream pipelines sabotage|Nord Stream I and Nord Stream II]] were damaged by explosives close to Bornholm in Denmark.<ref name=":5">{{Cite journal |last=de Jong |first=Moniek |date=January 2024 |title=Tracing the downfall of the Nord Stream 2 gas pipeline |url=https://wires.onlinelibrary.wiley.com/doi/10.1002/wene.502 |journal=WIREs Energy and Environment |language=en |volume=13 |issue=1 |doi=10.1002/wene.502 |bibcode=2024WIREE..13E.502D |issn=2041-8396}}</ref> In October 2023, the [[Balticconnector|Bal-ticconnector]] gas pipeline was damaged by the anchor of the Chinese container vessel [[Newnew Polar Bear|New New Polar Bear]].<ref>{{Cite report |url=https://digiriiul.sisekaitse.ee/handle/123456789/3591 |title=Security Threats to the Undersea Connections Related Critical Infrastructure of the Baltic States: Baltic Sea in the Focus of Hybrid Warfare |last1=Muuga |first1=Emilia |last2=Loik |first2=Ramon |last3=Kaup |first3=Georg-Henri |last4=Savimaa |first4=Raul |last5=Koort |first5=Erkki |date=2025 |publisher=Estonian Academy of Security Sciences |doi=10.15158/nv7t-kg46 |pages=9.975Mb |language=en}}</ref> In November 2024, telecoms cables were damaged, another case of suspected sabotage from a Chinese bulk carrier, departing from a Russian port.<ref>{{Cite web |date=2025-01-03 |title=Subsea Sabotage in the Baltic Sea - a Timeline for Perspective |url=https://www.marinelink.com/news/subsea-sabotage-baltic-sea-a-timeline-520782 |access-date=2025-05-26 |website=MarineLink |language=en}}</ref> In December 2024, a ship called [[Estlink|Estlink 2]], which is registered in the Cook Islands, is thought to be part of a Russian shadow fleet. It is suspected that this ship damaged internet cables.<ref>{{Cite news |last1=Lehto |first1=Essi |last2=Sytas |first2=Andrius |last3=Lehto |first3=Essi |last4=Sytas |first4=Andrius |date=2024-12-26 |title=Finland boards oil tanker suspected of causing internet, power cable outages |url=https://www.reuters.com/world/europe/finland-police-investigate-role-foreign-ship-after-power-cable-outage-2024-12-26/ |access-date=2025-05-26 |work=Reuters |language=en}}</ref> These incidents have led to responses from NATO, the European Union and national governments.<ref name=":7">{{Cite journal |last1=Bueger |first1=Christian |last2=Liebetrau |first2=Tobias |date=2023-09-01 |title=Critical maritime infrastructure protection: What's the trouble? |url=https://www.sciencedirect.com/science/article/pii/S0308597X23003056 |journal=Marine Policy |volume=155 |pages=105772 |doi=10.1016/j.marpol.2023.105772 |bibcode=2023MarPo.15505772B |issn=0308-597X}}</ref> NATO has increased its air and naval presence, as well as agreed to establish the Maritime Centre for the Security of Critical Undersea Infrastructure within NATO’s Allied Maritime Command (MARCOM), among other cooperation efforts.<ref name=":8">{{Cite report |url=https://www.jstor.org/stable/resrep55403 |title=NATO's Role in Protecting Critical Undersea Infrastructure |last1=Monaghan |first1=Sean |last2=Svendsen |first2=Otto |last3=Darrah |first3=Michael |last4=Arnold |first4=Ed |date=2023 |publisher=Center for Strategic and International Studies (CSIS)}}</ref> The EU has updated its Maritime Security Strategy, launched an action plan and a coordi-nation group for infrastructure protection, while national governments have strengthened surveil-lance, legal tools, and seabed defence capabilities.<ref name=":9">{{Cite journal |last=Loik |first=Ramon |date=2024-11-21 |title=Undersea Hybrid Threats in Strategic Competition: The Emerging Domain of NATO–EU Defense Cooperation |url=https://journalonbalticsecurity.com/journal/JOBS/article/126 |journal=Journal on Baltic Security |language=en |volume=10 |issue=2 |pages=1–25 |doi=10.57767/jobs_2024_008 |issn=2382-9222}}</ref> Aside from technical standards, political decisions influence what is deemed as “critical” infrastructure. Critical maritime infrastructure is deemed as critical since economies in today's society are dependent on this infrastructure.<ref>{{Cite web |title=More EU cooperation needed to mitigate risks to critical maritime infrastructure |url=https://eda.europa.eu/news-and-events/news/2023/05/04/stronger-eu-cooperation-needed-to-mitigate-risks-to-critical-maritime-infrastructure |access-date=2025-05-26 |website=eda.europa.eu |language=en}}</ref> Therefore, they require an extra layer of protection, whether by security policies or military protection.<ref name=":7" />

=== Hybrid warfare ===
In the current geopolitical climate, CMI is facing challenges posed by hybrid warfare threats.<ref name=":8" /> Hybrid threats in the Baltic Sea are often associated with Russian actions and operate below the official threshold of war, which poses a political challenge.<ref name=":12">{{Cite journal |last1=Schaub |first1=Gary |last2=Murphy |first2=Martin |last3=Hoffman |first3=Frank G |date=2017-01-02 |title=Hybrid Maritime Warfare: Building Baltic Resilience |url=https://www.tandfonline.com/doi/full/10.1080/03071847.2017.1301631 |journal=The RUSI Journal |language=en |volume=162 |issue=1 |pages=32–40 |doi=10.1080/03071847.2017.1301631 |issn=0307-1847}}</ref> The challenge posed by hybrid threats is that they operate in a grey area between peace and violence . For example, the Nord Stream pipeline sabotage demonstrated this problem by exploitation of legal ambiguities,<ref name=":7" /><ref name=":10">{{Citation |last1=Ringbom |first1=Henrik |title=Sabotage of Critical Offshore Infrastructure: a Case Study of the Balticconnector Incident |date=2024-07-27 |work=Maritime Security Law in Hybrid Warfare |pages=155–194 |url=https://brill.com/edcollchap/book/9789004707993/BP000019.xml |access-date=2025-05-26 |publisher=Brill Nijhoff |language=en |doi=10.1163/9789004707993_008 |isbn=978-90-04-70799-3 |last2=Lott |first2=Alexander}}</ref> the complexity of attribution, and the disruption of alliance cohesion.<ref name=":8" /> The incident highlights the vulnerability of criti-cal infrastructure and the absence of coherent political responses.<ref name=":8" /> Responding to hybrid threats requires sustained and coordinated efforts between civilian and military actors.<ref>{{Cite journal |last1=Metrick |first1=Andrew |last2=Hicks |first2=Kathleen H. |date=2018-03-12 |title=Contested Seas |url=https://www.csis.org/analysis/contested-seas |language=en}}</ref> However, the maritime domain presents unique difficulties, including jurisdictional overlaps, fragmented responsibilities, and the challenge of adapting land-based security frameworks to the sea.<ref name=":7" /> Hybrid tactics, such as uncrewed aerial vehicle (drone) surveillance, covert sabotage, and information manipulation, aim not only to damage infrastructure but also to undermine public trust and create strategic instability in the region.<ref name=":11">Swistek, G. and Paul, M. (2023) ''Geopolitics in the Baltic Sea region: The “Zeitenwende” in the context of critical maritime infrastructure, escalation threats and the German willingness to lead,'' SWP Comment, 9/2023. <nowiki>https://doi.org/10.18449/2023C09</nowiki>.</ref>

=== Geopolitical Dimensions of Critical Maritime Infrastructure ===
The Baltic Sea region in the post-Cold War era has for a long time been regarded as an area with little geopolitical tensions. With the Soviet presence in the south, the American influence through the NATO members Denmark and Germany and the neutral states Sweden and Finland, an equilibrium existed, often referred to as the “Nordic balance”. This balance also prolonged after the steady integration of the region into western institutions.<ref name=":12" />

However, in recent years this geopolitical reality has increasingly been challenged by the neo-imperial ambitions of Russia, manifesting itself in aggression against Ukraine. This development reached its peak with the full-scale invasion of the sovereign country in 2022. Also in the Baltic Sea has Russia pursued a strategy of regional dominance, designating the regional sea as a zone of strategic influence in its naval doctrine published in 2022. Yet, such a positioning in itself was significantly complicated by the accession of Sweden and Finland to NATO.<ref name=":11" /> 

Against this geopolitical background, it becomes clear, why many of the recent infrastructure projects in the Baltic Sea were subject to big political debates. Projects such as the [[Balticconnector]], which links the Finnish and Estonian gas markets and has been described by the European Commission as an expression of European solidarity,<ref>{{Cite web |title=Balticconnector gas pipeline up and running since 1 January 2020 - European Commission |url=https://commission.europa.eu/news/balticconnector-gas-pipeline-and-running-1-january-2020-2020-01-08_en |access-date=2025-05-27 |website=commission.europa.eu |language=en}}</ref> whilst the Gas Interconnection Poland–Lithuania (GIPL) which connects the Polish and Lithuanian gas networks,<ref>{{Cite web |title=Inauguration of gas interconnection between Poland and Lithuania |url=https://commission.europa.eu/news/inauguration-gas-interconnection-between-poland-and-lithuania-2022-05-05_en |access-date=2025-05-27 |website=commission.europa.eu |language=en}}</ref> and the development of multiple LNG terminals, have all played a significant role in reducing European reliance on Russian energy supplies.<ref name=":7" /> These initiatives form part of broader efforts to enhance regional integration and bring the Baltic Sea states into closer alignment with the European Union.<ref>{{Cite book |title=Technopolitics and the making of Europe: infrastructures of security |date=2024 |publisher=Routledge |isbn=978-1-032-21184-8 |editor-last=Klimburg-Witjes |editor-first=Nina |series=Emerging technologies, ethics and international affairs |location=Abingdon, Oxon ; New York, NY |editor-last2=Trauttmansdorff |editor-first2=Paul}}</ref> In contrast, the Nord Stream pipelines, particularly [[Nord Stream 2]], became a source of political controversy.<ref name=":5" /> Critics argued that the project would increase European dependence on Russian gas, bypass transit countries such as Ukraine and Poland, and undermine EU energy solidarity by strengthening Russia’s leverage over countries like Germany<ref>{{Citation |last1=Koivurova |first1=Timo |title=The Nord Stream Pipelines from the Viewpoint of Law and Geopolitics |date=2024-07-27 |work=Maritime Security Law in Hybrid Warfare |pages=195–221 |url=https://brill.com/edcollchap/book/9789004707993/BP000020.xml |access-date=2025-05-27 |publisher=Brill Nijhoff |language=en |doi=10.1163/9789004707993_009 |isbn=978-90-04-70799-3 |last2=Winkel |first2=Theresa}}</ref>.  Nord Stream 2 experienced prolonged delays and was ultimately suspended following the imposition of international sanctions against Russia after the invasion of Ukraine in 2022.<ref name=":5" /> In addition to political and economic controversies, the Nord Stream pipelines also became the subject of security-related concerns regarding their potential strategic implications in the Baltic Sea region.<ref name=":5" /> Prior to the 2022 sabotage of the Nord Stream pipelines, security experts and several Eastern European states had raised concerns that such infrastructure could be exploited by Russia for intelligence gathering and military purposes in the Baltic Sea.<ref name=":13">{{Cite journal |last=Schaller |first=Christian |date=2024-05-21 |title=Russia's Mapping of Critical Infrastructure in the North and Baltic Seas – International Law as an Impediment to Countering the Threat of Strategic Sabotage? |url=https://brill.com/view/journals/nord/93/2/article-p202_002.xml |journal=Nordic Journal of International Law |volume=93 |issue=2 |pages=202–236 |doi=10.1163/15718107-bja10083 |issn=0902-7351}}</ref> These concerns gained renewed attention following the sabotage incident, which highlighted challenges in the legal and regulatory frameworks governing the protection of critical infrastructure.<ref name=":7" /><ref name=":9" /><ref name=":10" /> The difficulty in conclusively attributing the attack also drew attention to the limitations of existing mechanisms for responding to hybrid threats in the maritime domain.<ref name=":8" /><ref name=":7" />

== Helsinki Convention ==

=== 1974 Convention ===
For the first time ever, all the sources of pollution around an entire sea were made subject to a single convention, signed in 1974 by the then seven Baltic coastal states. The 1974 Convention entered into force on 3 May 1980.

=== 1992 Convention ===
{{main|Helsinki Convention on the Protection of the Marine Environment of the Baltic Sea Area}}
In the light of political changes and developments in international environmental and maritime law, a new convention was signed in 1992 by all the states bordering on the Baltic Sea, and the European Community. After ratification, the [[Convention on the Protection of the Marine Environment of the Baltic Sea Area|Convention]] entered into force on 17 January 2000. The Convention covers the whole of the Baltic Sea area, including inland waters and the water of the sea itself, as well as the seabed. Measures are also taken in the whole catchment area of the Baltic Sea to reduce land-based pollution. The convention on the Protection of the Marine Environment of the Baltic Sea Area, 1992, entered into force on 17 January 2000.

The governing body of the convention is the [[HELCOM|Helsinki Commission]],<ref>[http://www.helcom.fi/home/en_GB/welcome/ Helcom : Welcome] {{webarchive |url=https://web.archive.org/web/20070506161857/http://www.helcom.fi/home/en_GB/welcome/ |date=6 May 2007 }}. Helcom.fi. Retrieved on 23 June 2011.</ref> also known as HELCOM, or Baltic Marine Environment Protection Commission. The present contracting parties are Denmark, Estonia, the European Community, Finland, Germany, Latvia, Lithuania, Poland, Russia, and Sweden.

The ratification instruments were deposited by the European Community, Germany, Latvia and Sweden in 1994, by Estonia and Finland in 1995, by Denmark in 1996, by Lithuania in 1997, and by Poland and Russia in November 1999.

== Coordination in the Baltic Sea region ==

=== European Union ===
The [[European Union]] (EU) is one core framework shaping regional security coordination in the [[Baltic region|Baltic Sea region.]] The EU has  recognised this area as one of thirteen designated zones for territorial cooperation. Following the accession of the [[Baltic states|Baltic States]] in 2004, the Baltic Sea is now considered an EU internal sea.<ref>{{Cite journal |last=Bengtsson |first=Rikard |title=An EU Strategy for the Baltic Sea region: good intentions meet complex challenges |journal=European Policy Analysis |volume=2009 |issue=9 |via=Swedish Institute for European Policy Studies}}</ref> The following initiatives form the basis of the EU's engagement in [[Maritime domain awareness|Maritime Domain Awareness (MDA)]] and Maritime Situational Awareness (MSA) in the Baltic Sea:

* '''2006''': Maritime Surveillance Network ('''MARSUR'''), a project aiming at facilitating communication between maritime information systems in Europe, that is undertaken by the European Defence Agency (EDA).<ref>{{Cite web |title=Maritime Surveillance (MARSUR) |url=https://eda.europa.eu/what-we-do/all-activities/activities-search/maritime-surveillance-(marsur) |access-date=2025-05-23 |website=European Defence Agency}}</ref> 
* '''2009''': Sea Surveillance Co-Operation Baltic Sea ('''SUCBAS'''), a Maritime Situational Awareness (MSA) cooperation between Baltic Sea countries with the objective of sharing information effectively.<ref>{{Cite web |title=SUCBAS Overview |url=https://sucbas.vercel.app/ |access-date=2025-05-25 |website=SUCBAS}}</ref> 
* '''2009''': EU Strategy for the Baltic Sea Region ('''EUSBSR'''), a macro-regional strategy that involves EU member states bordering the Baltic Sea and the EU Commission. The strategy is centred on four core pillars: the environment, prosperity, accessibility and maritime security.<ref>{{Cite web |title=EUSBSR - About |url=https://eusbsr.eu/about/ |access-date=2025-05-23 |website=EUSBSR}}</ref><ref>{{Cite journal |last1=Metzger |first1=Jonathan |last2=Schmitt |first2=Peter |date=2012-02-01 |title=When Soft Spaces Harden: The EU Strategy for the Baltic Sea Region |url=https://journals.sagepub.com/doi/10.1068/a44188 |journal=Environment and Planning A: Economy and Space |language=EN |volume=44 |issue=2 |pages=263–280 |doi=10.1068/a44188 |bibcode=2012EnPlA..44..263M |issn=0308-518X}}</ref><ref>{{Cite journal |last=COMMISSION OF THE EUROPEAN COMMUNITIES |title=European Union Strategy for the Baltic Sea Region - Action Plan |url=https://eusbsr.eu/wp-content/uploads/action-plan_2009_en.pdf |journal=Commission Staff Working Document |volume=2009 |issue=712}}</ref>
* '''2021-2027''': Interreg Baltic Sea Region, an EU co-funded transnational cooperation network.<ref>{{Cite web |title=Baltic Sea Region - Interreg EU |url=https://interreg.eu/programmes/baltic-sea-region/ |access-date=2025-05-25 |website=interreg.eu |language=en}}</ref><ref>{{Cite web |title=Interreg Baltic Sea Region - Solutions for a green and resilient Baltic Sea region |url=https://interreg-baltic.eu/about/ |access-date=2025-05-25 |website=Interreg Baltic Sea Region |language=en-US}}</ref>

=== NATO ===
The [[NATO|North Atlantic Treaty Organisation (NATO)]] is the primary provider of a [[collective defense]] system.<ref>{{Cite journal |last=Fałkowski |first=Andrzej |date=2021 |title=Building security in the Baltic Sea region: Military perspective and NATO approach |url=https://www.centrumbalticum.org/files/5104/BSR_Policy_Briefing_10_2021.pdf |journal=BSR Policy Briefing Series |volume=2021 |issue=10}}</ref> Following the accession of Finland in 2023 and Sweden in 2024, the majority of the states bordering the Baltic Sea have become members of NATO, simplifying the organisational geography of the region.<ref>{{Cite journal |last1=Alberque |first1=William |last2=and Schreer |first2=Benjamin |date=2022-05-04 |title=Finland, Sweden and NATO Membership |url=https://www.tandfonline.com/doi/full/10.1080/00396338.2022.2078046 |journal=Survival |volume=64 |issue=3 |pages=67–72 |doi=10.1080/00396338.2022.2078046 |issn=0039-6338}}</ref>

The following NATO initiatives and bodies are particularly relevant for the Baltic Sea region:

* '''2023''': Critical Undersea Infrastructure Coordination Cell, a centre aiming at connecting military and civilian stakeholders.<ref>{{Cite web |last=NATO |date=2023-02-15 |title=NATO stands up undersea infrastructure coordination cell |url=https://www.nato.int/cps/en/natohq/news_211919.htm |access-date=2025-05-25 |website=NATO |language=en}}</ref>
* '''2023''': Maritime Centre for the Security of Critical Undersea Infrastructure ('''NMCSCUI'''), a centre aiming at protecting the allies’ critical undersea infrastructure.<ref>{{Cite journal |last1=Monaghan |first1=Sean |last2=Svendsen |first2=Otto |last3=Darrah |first3=Michael |last4=Arnold |first4=Ed |date=2023 |title=NATO's Role in Protecting Critical Undersea Infrastructure |url=https://csis-website-prod.s3.amazonaws.com/s3fs-public/2023-12/231219_Monaghan_NATO_CUI.pdf?VersionId=6Usacn9I0OlKjF6t4s4XhehMIVROp74W |journal=CSIS Briefs}}</ref>
* '''2023''': EU-NATO Task Force on Resilience of Critical Infrastructure, a cooperation on increasing the resilience of [[critical infrastructure]], [[supply chain]]s and technology.<ref>{{Cite web |date=2023 |title=EU-NATO TASK FORCE ON THE RESILIENCE OF CRITICAL INFRASTRUCTURE - Final Assessment Report |url=https://commission.europa.eu/system/files/2023-06/EU-NATO_Final%20Assessment%20Report%20Digital.pdf |access-date=2025-05-22 |website=European Commission}}</ref>
* '''2025''': Baltic Sentry, a NATO [[military operation]] aiming at increasing the military presence in the Baltic Sea to improve the safety of critical infrastructure.<ref>{{Cite web |last=NATO |date=2025-01-14 |title=NATO launches 'Baltic Sentry' to increase critical infrastructure security |url=https://www.nato.int/cps/en/natohq/news_232122.htm |access-date=2025-05-23 |website=NATO |language=en}}</ref><ref>{{Cite journal |last=Hansen |first=Flemming Splidsboel |date=2025 |title=Russian military thinking about the Baltic Sea and the Arctic |url=https://pure.diis.dk/ws/files/26437168/russian-military-web.pdf |journal=DIIS Policy Brief |via=Danish Institute for International Studies (DIIS)}}</ref> 
* Baltic Operations ('''[[BALTOPS]]'''), a multinational naval manoeuvre that is held annually in the Baltic Sea.<ref>{{Cite web |date=2022-06-16 |title=Baltic Operations |url=https://www.bundeswehr.de/de/organisation/marine/uebungen/marine-manoever-baltops#:~:text=Was%20ist%20BALTOPS%20?,der%20Region%20als%20Gastland%20verkn%C3%BCpft |access-date=2025-05-25 |website=www.bundeswehr.de |language=de}}</ref>

=== Nordic Defence Cooperation ===
The [[Nordic Defence Cooperation|Nordic Defence Cooperation (NORDEFCO)]] is a [[military alliance]] comprising the [[Nordic countries]] of Denmark, Finland, Iceland, Norway and Sweden. It was established in 2009. The objectives of this cooperation structure include improving the national defense of each country, identifying shared strategic interests, and promoting the development of coordinated, effective responses. The strategy paper 'Vision 2025' outlines plans to enhance [[collaboration]] with the [[Baltic states]] and transatlantic allies.<ref>{{Cite web |title=About Nordefco |url=https://www.nordefco.org/the-basics-about-nordefco |access-date=2025-05-22 |website=www.nordefco.org}}</ref>

=== Council of the Baltic Sea States ===
The [[Council of the Baltic Sea States]] (CBSS) is an [[Intergovernmentalism|intergovernmental]] political organisation that focuses on regional cooperation. It was established in 1992. CBSS comprises ten European states and the [[European Union]].<ref>{{Cite web |last=CBSS |title=Member States |url=https://cbss.org/about-us/member-states/ |access-date=2025-05-25 |website=CBSS |language=en-US}}</ref> The organisation serves as a forum for political dialogue in the region and follows three main objectives: Regional Identity, Safe & Secure Region, and Sustainable & Prosperous Region. CBSS holds annual regional and international meetings.<ref>{{Cite web |last=CBSS |title=About Us |url=https://cbss.org/about-us/ |access-date=2025-05-25 |website=CBSS |language=en-US}}</ref>

== See also ==
{{portal|Oceans|Geography}}
<!-- Please keep entries in alphabetical order and add a short description [[WP:SEEALSO]] -->
{{div col|colwidth=20em|small=yes}}
* [[Baltic (disambiguation)]]
* [[Baltic region]]
* [[Baltic Sea Action Group]] (BSAG)
* [[Council of the Baltic Sea States]]
* [[List of cities and towns around the Baltic Sea]]
* [[List of rivers of the Baltic Sea]]<!--
* [[MS Estonia|MS ''Estonia'']]
* [[MS Jan Heweliusz|MS ''Jan Heweliusz'']]
* [[MV Goya|MV ''Goya'']]
* [[MV Wilhelm Gustloff|MV ''Wilhelm Gustloff'']]-->
* [[Nord Stream 1]]
* [[Nord Stream 2]]
* [[Northern Europe]]
* [[Ports of the Baltic Sea]]
* [[Scandinavia]]<!--
* [[SS Cap Arcona|SS ''Cap Arcona'']]
* [[SS Thielbek (1940)|SS ''Thielbek'']]
please keep entries in alphabetical order and add a short description -->
{{div col end}}

==Notes==
{{reflist|group=note}}

==References==
{{Reflist}}

===Bibliography===
* {{cite book|editor-last=Fairbridge |editor-first=Rhodes |title=The Encyclopedia of Oceanography| first=Pentti |last=Alhonen |chapter=Baltic Sea |pages=87–91 |location=New York |publisher=Van Nostrand Reinhold Company |year= 1966}}
* {{cite encyclopedia | article = BLACK SEA | last = Schmitt | first = Rüdiger | url = http://www.iranicaonline.org/articles/black-sea | encyclopedia  = Encyclopaedia Iranica, Vol. IV, Fasc. 3 | pages = 310–313 | year = 1989 | title = Black Sea – Encyclopaedia Iranica }}

==Further reading==
* [http://balticworlds.com/spatial-politics-fuzzy-regionalism/ Norbert Götz. "Spatial Politics and Fuzzy Regionalism: The Case of the Baltic Sea Area." ''Baltic Worlds'' 9 (2016) 3: 54–67.]
* Aarno Voipio (ed., 1981): "The Baltic Sea." Elsevier Oceanography Series, vol. 30, Elsevier Scientific Publishing, 418 p, {{ISBN|0-444-41884-9}}
* {{cite journal | last1 = Ojaveer | first1 = H. | last2 = Jaanus | first2 = A. | last3 = MacKenzie | first3 = B. R. | last4 = Martin | first4 = G. | last5 = Olenin | first5 = S. | display-authors = etal   | year = 2010 | title = Status of Biodiversity in the Baltic Sea | journal = [[PLoS ONE]] | volume = 5 | issue = 9| page = e12467 | doi = 10.1371/journal.pone.0012467 | pmid = 20824189 | pmc = 2931693 | bibcode = 2010PLoSO...512467O | doi-access = free }}
* {{cite book|last1=Peter|first1=Bruce|title=Baltic Ferries|date=2009|publisher=Ferry Publications|location=Ramsey, Isle of Man|isbn=9781906608057}}
* {{cite book|author=((The BACC II Author Team)) |display-authors=etal |title=Second Assessment of Climate Change for the Baltic Sea Basin |publisher=Springer |year=2015 |isbn= 978-3-319-16006-1 |doi=10.1007/978-3-319-16006-1|series=Regional Climate Studies|bibcode=2015sacc.book.....T |s2cid=127011711 |url=http://www.oapen.org/search?identifier=1002057}} <!--Open Access-->

===Historical===
* Bogucka, Maria. "The Role of Baltic Trade in European Development from the XVIth to the XVIIIth Centuries". ''Journal of European Economic History'' 9 (1980): 5–20.
* Davey, James. ''The Transformation of British Naval Strategy: Seapower and Supply in Northern Europe, 1808–1812'' (Boydell, 2012).
* {{Cite EB1911|wstitle= Baltic Sea | volume= 3 |last1= Dickson |first1= Henry Newton |author1-link= Henry Newton Dickson | pages = 286&ndash;287 |short=1}}
* Fedorowicz, Jan K. ''England's Baltic Trade in the Early Seventeenth Century: A Study in Anglo-Polish Commercial Diplomacy'' (Cambridge UP, 2008).
* Frost, Robert I. ''The Northern Wars: War, State, and Society in Northeastern Europe, 1558–1721'' (Longman, 2000).
* Grainger, John D. ''The British Navy in the Baltic'' (Boydell, 2014).
* Kent, Heinz S. K. ''War and Trade in Northern Seas: Anglo-Scandinavian Economic Relations in the Mid Eighteenth Century'' (Cambridge UP, 1973).
* Koningsbrugge, Hans van. "In War and Peace: The Dutch and the Baltic in Early Modern Times". ''Tijdschrift voor Skandinavistiek'' 16 (1995): 189–200.
* Lindblad, Jan Thomas. "Structural Change in the Dutch Trade in the Baltic in the Eighteenth Century". ''Scandinavian Economic History Review'' 33 (1985): 193–207.
* Lisk, Jill. ''The Struggle for Supremacy in the Baltic, 1600–1725'' (U of London Press, 1967).
* {{Cite book |last=Niktalab |first=Poopak |author-link=Poopak NikTalab |title=Over the Alps: History of Children and Youth literature in Europe (Chapter 2 Baltic sails: the evolution of children's and youth literature in the Baltic countries) |publisher=Faradid Publisher |year=2024 |isbn=9786225740457 |edition=1st |location=Tehran, Iran |pages=85–124 |language=fa}}
* Roberts, Michael. ''The Early Vasas: A History of Sweden, 1523–1611'' (Cambridge UP, 1968).
* Rystad, Göran, Klaus-R. Böhme, and Wilhelm M. Carlgren, eds. ''In Quest of Trade and Security: The Baltic in Power Politics, 1500–1990.'' Vol. 1, 1500–1890. Stockholm: Probus, 1994.
* Salmon, Patrick, and Tony Barrow, eds. ''Britain and the Baltic: Studies in Commercial, Political and Cultural Relations'' (Sunderland University Press, 2003).
* Stiles, Andrina. ''Sweden and the Baltic 1523–1721'' (1992).
* Thomson, Erik. "Beyond the Military State: Sweden's Great Power Period in Recent Historiography". ''History Compass'' 9 (2011): 269–283. {{doi|10.1111/j.1478-0542.2011.00761.x}}
* Tielhof, Milja van. The "Mother of All Trades": The Baltic Grain Trade in Amsterdam from the Late 16th to Early 19th Century. Leiden, The Netherlands: Brill, 2002.
* Warner, Richard. "British Merchants and Russian Men-of-War: The Rise of the Russian Baltic Fleet". In Peter the Great and the West: New Perspectives. Edited by Lindsey Hughes, 105–117. Basingstoke, UK: Palgrave Macmillan, 2001.

== External links ==
{{Commons category}}
{{AmCyc poster|Baltic Sea}}
{{EB1911 poster|Baltic Sea}}
* [https://web.archive.org/web/20160303225024/http://www.smhi.se/sgn0102/n0205/havsomr/havsomr_plansch.pdf The Baltic Sea, Kattegat and Skagerrak – sea areas and draining basins, poster with integral information by the Swedish Meteorological and Hydrological Institute]
* [https://web.archive.org/web/20071023052150/http://www.baltic.vtt.fi/demo/baltmap.htm Baltic Sea clickable map and details.]
* [https://web.archive.org/web/20070911174644/http://www.balticsea.lt/en Protect the Baltic Sea while it's still not too late.]
* [https://archive.today/20120728165223/http://www.balticseaportal.fi/ The Baltic Sea Portal] – a site maintained by the{{cite web|url=http://www.fimr.fi/en.html |title=Finnish Institute of Marine Research |access-date=15 July 2007 |url-status=dead |archive-url=https://web.archive.org/web/20080214115037/http://www.fimr.fi/en.html |archive-date=14 February 2008 }} (FIMR) (in English, Finnish, Swedish and Estonian)
* [https://web.archive.org/web/20110625011603/http://www.balticnest.org/ www.balticnest.org]
* [https://web.archive.org/web/20050317135023/http://depts.washington.edu/baltic/encyclopedia.html Encyclopedia of Baltic History]
* [https://web.archive.org/web/20120912164106/http://www.abc.se/~pa/uwa/wrecks.htm Old shipwrecks] in the Baltic
* [https://web.archive.org/web/20071212134140/http://www.pgi.gov.pl/pgi_en/index.php?option=news&task=viewarticle&sid=4&Itemid=2 How the Baltic Sea was changing] – Prehistory of the Baltic from the [http://www.pgi.gov.pl/ Polish Geological Institute]
* [http://www.helsinki.fi/maantiede/geofi/fennia/demo/pages/oksanen.htm Late Weichselian and Holocene shore displacement history of the Baltic Sea in Finland] – more prehistory of the Baltic from the [http://www.helsinki.fi/geography/ Department of Geography] of the [[University of Helsinki]]
* [https://web.archive.org/web/20040603121723/http://maps.grida.no/baltic/ Baltic Environmental Atlas: Interactive map of the Baltic Sea region]
* [http://www.spiegel.de/international/europe/0,1518,524139,00.html Can a New Cleanup Plan Save the Sea? – ''spiegel.de'']
* [https://web.archive.org/web/20060903112114/http://www.ferrylines.com/en/routes/ferries-in-the-baltic-sea/ List of all ferry lines in the Baltic Sea]
* [https://web.archive.org/web/20170731171716/http://www.helcom.fi/ The Helsinki Commission (HELCOM)] HELCOM is the governing body of the "Convention on the Protection of the Marine Environment of the Baltic Sea Area"
* [http://www.baltice.org/ Baltice.org] – information related to winter navigation in the Baltic Sea.
* [https://web.archive.org/web/20081205101019/http://www.balticseawind.org/ Baltic Sea Wind] – Marine weather forecasts
* [https://web.archive.org/web/20090831081653/http://andreaskiel.blip.tv/file/2323160 Ostseeflug] – A short film (55'), showing the coastline and the major German cities at the Baltic sea.

{{List of seas}}
{{Marginal seas of the Atlantic Ocean}}
{{Countries bordering the Baltic Sea}}
{{Islands in the Baltic Sea}}
{{Polish coast|state=autocollapse}}
{{Saint Petersburg}}

{{Authority control}}

[[Category:Baltic Sea| ]]
[[Category:Baltic region]]
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[[Category:Federal waterways in Germany]]
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[[Category:Bodies of water of Estonia]]
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[[Category:Bodies of water of Poland]]
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[[Category:Bodies of water of Leningrad Oblast]]
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